ORCID Profile
0000-0003-2528-417X
Current Organisations
Curtin University
,
University of Western Australia
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Research Topics
In Research Link Australia (RLA), "Research Topics" refer to ANZSRC FOR and SEO codes. These topics are either sourced from ANZSRC FOR and SEO codes listed in researchers' related grants or generated by a large language model (LLM) based on their publications.
Top 5 Research Topics
ANZSRC Field of Research (FoR)
Geology | Geochronology | Petroleum and Coal Geology | Ore Deposit Petrology | Geochemistry | Inorganic Geochemistry | Geotectonics | Isotope Geochemistry | Geophysics Not Elsewhere Classified | Sedimentology | Geochronology | Astronomical and Space Sciences | Geomagnetism | Organic Geochemistry | Extraterrestrial Geology | Animal Neurobiology | Functional Materials | Mineral Processing/Beneficiation | Crop and Pasture Biochemistry and Physiology | Land Capability and Soil Degradation | Medical Parasitology | Planetary Science (excl. Extraterrestrial Geology) | Stratigraphy (incl. Biostratigraphy and Sequence Stratigraphy) | Volcanology | Tectonics
ANZSRC Socio-Economic Objective (SEO)
Mineral Exploration not elsewhere classified | Oil and Gas Exploration | Expanding Knowledge in the Earth Sciences | Precious (Noble) Metal Ore Exploration | Primary Mining and Extraction of Mineral Resources not elsewhere classified | Earth sciences | Iron Ore Exploration | Mining and Extraction of Energy Resources not elsewhere classified | Wheat | Nervous System and Disorders | Climate change | Environmentally Sustainable Mineral Resource Activities not elsewhere classified | Expanding Knowledge in the Environmental Sciences | Mining and Extraction of Iron Ores | Infectious Diseases |
Related Links
Publications
Ion microprobe U–Pb zircon geochronology of a late tectonic granitic–gabbroic rock complex within the Hercynian Iberian belt
Publisher: Cambridge University Press (CUP)
Date: 09-11-2006
DOI: 10.1017/S0016756806002652
Abstract: Ion microprobe (SIMS) dating shows that three plutonic rock bodies representative of the major, ∼15 000 km 2 , late tectonic (late-D 3 ), plutonic rock series in the Central Iberian Zone of the Hercynian belt in west-central Iberia have indistinguishable zircon crystallization ages. Ledrada biotite granite and Colmenar cordierite-bearing biotite granite show gradual transitions in field appearance, petrography and chemistry and have statistically indistinguishable weighted average ages of 306.8 ± 1.9(2σ) Ma and 306.5 ± 1.5(2σ) Ma, respectively, which indicates that they originated during a single event involving a heterogeneous magma which notably varied in Al-content. The third rock body, Navahermosa meta-gabbronorite, has a weighted average zircon crystallization age of 305.6 ± 1.4(2σ) Ma, statistically indistinguishable (variance analysis, F-test, α = 0.05) from the granites. Zircon crystals in the gabbronoritic rock are anhedral, skeletal, millimetre-sized and partake in main magmatic textures, whereas the zircon grains in the granites are of more common appearance, much smaller, usually euhedral and enclosed in main magmatic crystals. As gestation times of granitic zircon, the time between zircon crystallization and magmatic intrusion, may be up to 5 Myr, the crystallization age of the gabbronoritic zircon may be the best estimate of the time of emplacement of the magmatic complex. Our study indicates co-existence of basic and silicic magmas in the Hercynian crustal section at c . 306 Ma, suggesting common genetic control. The two granitic rocks carry inherited zircon ranging from c. 1300 to 330 Ma, indicating that pre-Hercynian basement rocks of Proterozoic to Palaeozoic age contributed to the granitic magma.
The age distribution of detrital zircons in quartzites from the Toodyay-Lake Grace Domain, Western Australia: Implications for the early evolution of the Yilgarn Craton
Publisher: American Journal of Science (AJS)
Date: 11-2010
DOI: 10.2475/09.2010.13
Effectiveness of physiotherapy for lateral epicondylitis: a systematic review
Publisher: Informa UK Limited
Date: 2003
DOI: 10.1080/07853890310004138
Abstract: To evaluate the available evidence of the effectiveness of physiotherapy for lateral epicondylitis of the elbow. Randomised controlled trials (RCTs) identified by a highly sensitive search strategy in six databases in combination with reference checking. Two independent reviewers selected RCTs that included a physiotherapy intervention, patients with lateral epicondylitis, and at least one clinically relevant outcome measure. No language restrictions were made. Methodological quality was independently assessed by two blinded reviewers. A best evidence synthesis, including a quantitative and qualitative analysis, was conducted, weighting the studies with respect to their internal validity, statistical significance, clinical relevance, and statistical power. 23 RCTs were included in the review, evaluating the effects of lasertherapy, ultrasound treatment, electrotherapy, and exercises and mobilisation techniques. Fourteen studies satisfied at least 50% of the internal validity criteria. Except for ultrasound, pooling of data from RCTs was not possible because of insufficient data, or clinical or statistical heterogeneity. The pooled estimate of the treatment effects of two studies on ultrasound compared to placebo ultrasound, showed statistically significant and clinically relevant differences in favour of ultrasound. There is insufficient evidence either to demonstrate benefit or lack of effect of lasertherapy, electrotherapy, exercises and mobilisation techniques for lateral epicondylitis. Despite the large number of studies, there is still insufficient evidence for most physiotherapy interventions for lateral epicondylitis due to contradicting results, insufficient power, and the low number of studies per intervention. Only for ultrasound, weak evidence for efficacy was found. More better designed, conducted and reported RCTs are needed.
U-Pb and Pb-Pb zircon ages for metamorphic rocks in the Kaoko Belt of Northwestern Namibia: A Palaeo- to Mesoproterozoic basement reworked during the Pan-African orogeny
Publisher: Geological Society of South Africa
Date: 09-2004
DOI: 10.2113/107.3.455
SHRIMP zircon age for an Early Cambrian dolerite dyke: An intrusive phase of the Antrim Plateau Volcanics of northern Australia
Publisher: Informa UK Limited
Date: 12-2000
High-precision dating of the Kalkarindji large igneous province, Australia, and synchrony with the Early-Middle Cambrian (Stage 4-5) extinction
Publisher: Geological Society of America
Date: 06-2014
DOI: 10.1130/G35434.1
Climate‐induced changes in the suitable habitat of cold‐water corals and commercially important deep‐sea fishes in the North Atlantic
Publisher: Wiley
Date: 20-02-2020
DOI: 10.1111/GCB.14996
The affinity of Archean crust on the Yilgarn-Albany-Fraser Orogen boundary: Implications for gold mineralisation in the Tropicana Zone
Publisher: Elsevier BV
Date: 09-2015
Geology and geochronology of the Paleoproterozoic Hart Dolerite, Western Australia
Publisher: Elsevier BV
Date: 12-2019
Uplift of the Lüliang Mountains at ca. 5.7 Ma: Insights from provenance of the Neogene eolian red clay of the eastern Chinese Loess Plateau
Publisher: Elsevier BV
Date: 08-2018
Untying the Kibaran knot: A reassessment of Mesoproterozoic correlations in southern Africa based on SHRIMP U-Pb data from the Irumide belt
Publisher: Geological Society of America
Date: 2003
Proterozoic basic magmatism of the Siberian Craton: Main stages and their geodynamic interpretation
Publisher: Pleiades Publishing Ltd
Date: 07-2012
Adding pieces to the puzzle: episodic crustal growth and a new terrane in the northeast Yilgarn Craton, Western Australia
Publisher: Informa UK Limited
Date: 07-2012
Monazite trumps zircon: applying SHRIMP U–Pb geochronology to systematically evaluate emplacement ages of leucocratic, low-temperature granites in a complex Precambrian orogen
Publisher: Springer Science and Business Media LLC
Date: 07-07-2017
The Mesoproterozoic thermal evolution of the Musgrave Province in central Australia — Plume vs. the geological record
Publisher: Elsevier BV
Date: 06-2015
Provenance of the Ordovician–lower Silurian Tumblagooda Sandstone, Western Australia
Publisher: Informa UK Limited
Date: 03-10-2015
Zircon Lu-Hf isotopes and granite geochemistry of the Murchison Domain of the Yilgarn Craton: Evidence for reworking of Eoarchean crust during Meso-Neoarchean plume-driven magmatism
Publisher: Elsevier BV
Date: 09-2012
A one-billion-year gap in the Precambrian history of the southern Siberian Craton and the problem of the Transproterozoic supercontinent
Publisher: American Journal of Science (AJS)
Date: 11-2010
DOI: 10.2475/09.2010.03
The burning heart — The Proterozoic geology and geological evolution of the west Musgrave Region, central Australia
Publisher: Elsevier BV
Date: 2015
Conservative treatments for tennis elbow do subgroups of patients respond differently?
Publisher: Oxford University Press (OUP)
Date: 27-08-2007
DOI: 10.1093/RHEUMATOLOGY/KEM192
Abstract: To determine if subgroups of patients with tennis elbow respond differently in treatment. This study used in idual patient data (n = 383) from two randomized controlled trials that investigated a wait-and-see policy, corticosteroid injections and physiotherapy. Common outcome measures were: pain severity, global improvement, severity assessed by a blinded assessor, elbow disability and pain free grip strength. Subgroup analyses for previous history of elbow pain, baseline pain severity, duration of the current episode and employment status were performed at 6 and 52 weeks. Patients' age, previous elbow symptoms and baseline pain severity were similar between trials, but other characteristics differed between trial populations. Based on in idual patient data from both trials, we found that corticosteroid injections were statistically and clinically superior at 6 weeks, but significantly worse at 52 weeks compared with both wait-and-see and physiotherapy. Subgroup effects were scarce and small. Patients with higher baseline pain score showed less benefit on pain outcomes between physiotherapy and a wait-and-see policy at 6 weeks. It also appeared that non-manual workers who had an injection were the only work subgroup to follow the general trend that injections were significantly worse than a wait-and-see policy on global improvement at 52 weeks. The treatment outcomes were largely similar between trials and not different between most subgroups studied. In tennis elbow, it would appear that patient characteristics play only a small role in predicting treatment outcomes, which supports the generalizability of in idual trial results.
Viewpoints in bioerosion research—are we really disagreeing? A reply to the comment by Silbiger and DeCarlo (2017)
Publisher: Oxford University Press (OUP)
Date: 03-10-2017
Co-phasing the planet formation imager
Publisher: SPIE
Date: 04-08-2016
DOI: 10.1117/12.2231081
Late Mesozoic tectonics of Central Asia based on paleomagnetic evidence
Publisher: Elsevier BV
Date: 09-2010
Evidence for Mesoarchean (∼3.2Ga) rifting of the Pilbara Craton: The missing link in an early Precambrian Wilson cycle
Publisher: Elsevier BV
Date: 02-2010
Zircon geochronology and partial structural re-interpretation of the late Archaean Mashaba Igneous Complex, south-central Zimbabwe
Publisher: Geological Society of South Africa
Date: 12-2007
Age and significance of voluminous mafic-ultramafic magmatic events in the Murchison Domain, Yilgarn Craton
Publisher: Informa UK Limited
Date: 07-2010
Geochronological constraints on nickel metallogeny in the Lake Johnston belt, Southern Cross Domain
Publisher: Informa UK Limited
Date: 22-07-2014
A Sequence of Pan-African and Hercynian Events Recorded in Zircons from an Orthogneiss from the Hercynian Belt of Western Central Iberia-an Ion Microprobe U-Pb Study
Publisher: Oxford University Press (OUP)
Date: 02-07-2004
Reply to the comment: Mantle plume-, but not arc-related Neoproterozoic magmatism in South China
Publisher: Elsevier BV
Date: 07-2004
A new Paleoproterozoic tectonic history of the eastern Capricorn Orogen, Western Australia, revealed by U–Pb zircon dating of micro-tuffs
Publisher: Elsevier BV
Date: 11-2016
SHRIMP U–Pb zircon age for the Segwagwa–Masoke Igneous Complex of southeastern Botswana and implications for the deformation history of the Achaean to Proterozoic Transvaal Supergroup of southern Afri
Publisher: Elsevier BV
Date: 06-2009
On the edge: U–Pb, Lu–Hf, and Sm–Nd data suggests reworking of the Yilgarn craton margin during formation of the Albany-Fraser Orogen
Publisher: Elsevier BV
Date: 06-2011
Transformation of an Archean craton margin during Proterozoic basin formation and magmatism: The Albany-Fraser Orogen, Western Australia
Publisher: Elsevier BV
Date: 09-2015
Proterozoic granulite formation driven by mafic magmatism: An example from the Fraser Range Metamorphics, Western Australia
Publisher: Elsevier BV
Date: 2014
A-type leucogranite magmatism in the evolution of continental crust on the western margin of the Siberian craton
Publisher: GeoScienceWorld
Date: 2007
DOI: 10.1016/J.RGG.2006.12.002
Abstract: We discuss problems of the origin, settings, and age of Neoproterozoic A-type leucogranites widespread in the Yenisei Ridge. Combined analysis of geological, petrological, and geochemical (including isotope) data shows that some granitoids (Glushikha complex) were formed at the postcollisional stage (750–720 Ma), and others (Tatarka complex), in an anorogenic environment (680–630 Ma). The anorogenic complex contains erse igneous rocks, including alkaline varieties and carbonatites. Leucogranites form separate plutons within different igneous complexes. They have high contents of potassium (up to ultrapotassic composition in the Glushikha complex), iron, and fluorine and are depleted in europium. Postcollisional granitoids show the highest concentrations of Rb, Th, and U, extremely low concentrations of Ba and Sr, whereas anorogenic granitoids are rich in Ta, Nb, Y, Sm, and HREE. The obtained data point to the augmented mantle contribution to the formation of continental crust of the Yenisei Ridge between 750 and 630 Ma. We also report new results of U-Pb zircon dating, including SHRIMP and Ar-Ar data.
New data on the age and protolith of granulites of the Olkhon collisional system (Baikal Region)
Publisher: Pleiades Publishing Ltd
Date: 04-2008
Revised geochronology of magmatism in the western Capricorn Orogen at 1805-1785 Ma: diachroneity of the Pilbara-Yilgarn collision
Publisher: Wiley
Date: 12-2003
Paleomagnetism of the 765 Ma Luakela volcanics in Northwest Zambia and implications for Neoproterozoic positions of the Congo Craton
Publisher: American Journal of Science (AJS)
Date: 12-2010
DOI: 10.2475/10.2010.05
Dense cold‐water coral garden of Paragorgia johnsoni suggests the importance of the Mid‐Atlantic Ridge for deep‐sea biodiversity
Publisher: Wiley
Date: 24-11-2021
DOI: 10.1002/ECE3.8319
Abstract: Mid‐ocean ridges generate a myriad of physical oceanographic processes that favor the supply of food and nutrients to suspension‐ and filter‐feeding organisms, such as cold‐water corals and deep‐sea sponges. However, the pioneering work conducted along the Mid‐Atlantic Ridge failed to report the presence of large and dense living coral reefs, coral gardens, or sponge aggregations. Here, we describe the densest, near‐natural, and novel octocoral garden composed of large red and white colonies of Paragorgia johnsoni Gray, 1862 discovered at 545–595 m depth on the slopes of the Mid‐Atlantic Ridge, in the Azores region. This newly discovered octocoral garden is a good candidate for protection since it fits many of the FAO criteria that define what constitutes a Vulnerable Marine Ecosystem. The observations described here corroborate the existence of a close relationship between the octocoral structure and the ambient currents on ridge‐like topographies, providing new insights into the functioning of mid‐ocean ridges' ecosystems. The ubiquitous presence of biogenic and geological topographies associated with mid‐ocean ridges, which could act as climate refugia, suggests their global importance for deep‐sea bio ersity. A better understanding of the processes involved is, therefore, required. Our observations may inspire future deep‐sea research initiatives to narrow existing knowledge gaps of biophysical connections with benthic fauna at small spatial scales along mid‐ocean ridges.
The petrogenesis of sodic granites in the Niujuanzi area and constraints on the Paleozoic tectonic evolution of the Beishan region, NW China
Publisher: Elsevier BV
Date: 07-2016
Using in situ SHRIMP U-Pb monazite and xenotime geochronology to determine the age of orogenic gold mineralization: An example from the Paulsens Mine, Southern Pilbara Craton
Publisher: Society of Economic Geologists
Date: 06-2017
Crystal orientation effects during ion microprobe U-Pb analysis of baddeleyite
Publisher: Elsevier BV
Date: 07-2000
Proterozoic Dyke Swarms of the Siberian Craton and Their Geodynamic Implications
Publisher: Wiley
Date: 10-2016
SHRIMP baddeleyite age for the Fraser Dyke Swarm, southeast Yilgarn Craton, Western Australia
Publisher: Informa UK Limited
Date: 04-2000
Geochronology and paleomagnetism of mafic igneous rocks in the Olenek Uplift, northern Siberia: Implications for Mesoproterozoic supercontinents and paleogeography
Publisher: Elsevier BV
Date: 05-2009
Using the isotope dating of endocontact hybrid rocks for the age determination of mafic rocks (southern Siberian craton)
Publisher: GeoScienceWorld
Date: 11-2013
DOI: 10.1016/J.RGG.2013.10.001
Abstract: Geological observations and petrological and geochemical criteria are used to detect hybrid rocks at the endocontact of a dolerite dike. The hybrid rocks were produced when the material of a mafic intrusion mixed with a felsic melt. The latter was produced by the melting of the metamorphic rocks making up the Goloustnaya basement inlier of the Siberian craton, under the thermal effect of the intruded dike. Two age groups of zircon have been identified in the hybrid rock by SHRIMP analysis. The Paleoproterozoic age of inherited zircon (1902, 1864, 1859, and 1855 Ma) reflects the contribution of ancient sources to the hybrid-rock composition. The young, primary-magmatic, zircon grains, produced by melting at the endocontact of the mafic intrusion (494 ± 5 Ma), are coeval with the hybrid rocks, and their age indicates when the mafic rocks intruded the metamorphic framework. Dikes of close age, with similar geochemical characteristics, are present on the vast southern margin of the Siberian craton—from Goloustnaya to Biryusa salients.
Long-lived, autochthonous development of the archean murchison domain, and implications for yilgarn craton tectonics
Publisher: Elsevier BV
Date: 05-2013
Early Neoproterozoic magmatism (1000â910 Ma) of the Zadinian and Mayumbian Groups (Bas-Congo): onset of Rodinia rifting at the western edge of the Congo craton
Publisher: Elsevier BV
Date: 08-2001
Electrotherapy modalities for lateral elbow pain
Publisher: Wiley
Date: 06-06-2018
Tracking sediment dispersal during orogenesis: A zircon age and Hf isotope study from the western Amadeus Basin, Australia
Publisher: Elsevier BV
Date: 09-2015
Piggy-back Supervolcanoes—Long-Lived, Voluminous, Juvenile Rhyolite Volcanism in Mesoproterozoic Central Australia
Publisher: Oxford University Press (OUP)
Date: 04-2015
STARD 2015: An Updated List of Essential Items for Reporting Diagnostic Accuracy Studies
Publisher: Oxford University Press (OUP)
Date: 12-2015
DOI: 10.1373/CLINCHEM.2015.246280
Abstract: Incomplete reporting has been identified as a major source of avoidable waste in biomedical research. Essential information is often not provided in study reports, impeding the identification, critical appraisal, and replication of studies. To improve the quality of reporting of diagnostic accuracy studies, the Standards for Reporting of Diagnostic Accuracy Studies (STARD) statement was developed. Here we present STARD 2015, an updated list of 30 essential items that should be included in every report of a diagnostic accuracy study. This update incorporates recent evidence about sources of bias and variability in diagnostic accuracy and is intended to facilitate the use of STARD. As such, STARD 2015 may help to improve completeness and transparency in reporting of diagnostic accuracy studies.
Early Palaeozoic orogenic collapse and voluminous late-tectonic magmatism in Dronning Maud Land and Mozambique: insights into the partially delaminated orogenic root of the East African–Antarctic Orog
Publisher: Geological Society of London
Date: 2008
DOI: 10.1144/SP308.3
Neoproterozoic granitoids in South China: Crustal melting above a mantle plume at ca. 825 Ma?
Publisher: Elsevier BV
Date: 10-04-2003
Corrigendum to “The burning heart — The Proterozoic geology and geological evolution of the west Musgrave Region, central Australia” [Gondwana Res., Volume 27, Issue 1, January 2015, Pages 64–94]
Publisher: Elsevier BV
Date: 10-2015
Effectiveness of exercise therapy: A best-evidence summary of systematic reviews
Publisher: Elsevier BV
Date: 2005
DOI: 10.1016/S0004-9514(05)70036-2
Abstract: The purpose of this project was to summarise the available evidence on the effectiveness of exercise therapy for patients with disorders of the musculoskeletal, nervous, respiratory, and cardiovascular systems. Systematic reviews were identified by means of a comprehensive search strategy in 11 bibliographic databases (08/2002), in combination with reference tracking. Reviews that included (i) at least one randomised controlled trial investigating the effectiveness of exercise therapy, (ii) clinically relevant outcome measures, and (iii) full text written in English, German or Dutch, were selected by two reviewers. Thirteen independent and blinded reviewers participated in the selection, quality assessment and data-extraction of the systematic reviews. Conclusions about the effectiveness of exercise therapy were based on the results presented in reasonable or good quality systematic reviews (quality score > or = 60 out of 100 points). A total of 104 systematic reviews were selected, 45 of which were of reasonable or good quality. Exercise therapy is effective for patients with knee osteoarthritis, sub-acute (6 to 12 weeks) and chronic (> or = 12 weeks) low back pain, cystic fibrosis, chronic obstructive pulmonary disease, and intermittent claudication. Furthermore, there are indications that exercise therapy is effective for patients with ankylosing spondylitis, hip osteoarthritis, Parkinson's disease, and for patients who have suffered a stroke. There is insufficient evidence to support or refute the effectiveness of exercise therapy for patients with neck pain, shoulder pain, repetitive strain injury, rheumatoid arthritis, asthma, and bronchiectasis. Exercise therapy is not effective for patients with acute low back pain. It is concluded that exercise therapy is effective for a wide range of chronic disorders.
Grain size matters: Implications for element and isotopic mobility in titanite
Publisher: Elsevier BV
Date: 06-2016
Models of Rodinia assembly and fragmentation
Publisher: Geological Society of London
Date: 2003
Palaeomagnetic constraints on the Proterozoic tectonic evolution of Australia
Publisher: Geological Society of London
Date: 2003
Early Ordovician CA-IDTIMS U–Pb zircon dating and conodont biostratigraphy, Canning Basin, Western Australia
Publisher: Informa UK Limited
Date: 02-01-2018
Updated Digital Map of Mafic Dyke Swarms and Large Igneous Provinces in Western Australia
Publisher: Wiley
Date: 10-2016
Zircon Ages from the Baydrag Block and the Bayankhongor Ophiolite Zone: Time Constraints on Late Neoproterozoic to Cambrian Subduction‐ and Accretion‐Related Magmatism in Central Mongolia
Publisher: University of Chicago Press
Date: 07-2009
DOI: 10.1086/598947
Shrimp baddeleyite and zircon ages for an Umkondo dolerite sill, Nyanga Mountains, Eastern Zimbabwe
Publisher: Geological Society of South Africa
Date: 03-2001
DOI: 10.2113/104.1.13
Genesis of the 1.21 Ga Marnda Moorn large igneous province by plume–lithosphere interaction
Publisher: Elsevier BV
Date: 02-2014
Paleomagnetic pole from the yilgarn B (YB) dykes of Western Australia: No Longer relevant to Rodinia reconstructions
Publisher: Elsevier BV
Date: 04-2001
Geology and age of the Glikson impact structure, Western Australia
Publisher: Informa UK Limited
Date: 09-2005
Palaeozoic arc magmatism in the Central Asian Orogenic Belt of Kazakhstan: SHRIMP zircon ages and whole-rock Nd isotopic systematics
Publisher: Elsevier BV
Date: 03-2008
Ion microprobe baddeleyite and zircon ages for Late Archaean mafic dykes of the Pilbara Craton, Western Australia
Publisher: Informa UK Limited
Date: 08-1999
Spatio-temporal constraints on lithospheric development in the southwest-central Yilgarn Craton, Western Australia
Publisher: Informa UK Limited
Date: 07-2012
Regional-scale polydiapirism predating the Neoarchean Yilgarn Orogeny
Publisher: Elsevier BV
Date: 03-2020
The geochronological framework of the Irumide Belt: A prolonged crustal history along the margin of the Bangweulu Craton
Publisher: American Journal of Science (AJS)
Date: 02-2009
DOI: 10.2475/02.2009.03
Devil in the detail; The 1150–1000Ma magmatic and structural evolution of the Ngaanyatjarra Rift, west Musgrave Province, Central Australia
Publisher: Elsevier BV
Date: 12-2010
Palaeomagnetic results from the Lancer 1 stratigraphic drillhole, Officer Basin, Western Australia, and implications for Rodinia reconstructions
Publisher: Informa UK Limited
Date: 06-2007
SHRIMP zircon dating and Nd isotopic systematics of Palaeoproterozoic migmatitic orthogneisses in the Epupa Metamorphic Complex of northwestern Namibia
Publisher: Elsevier BV
Date: 11-2010
Extension in high-grade terranes of the southern Omineca Belt, British Columbia: Evidence from paleomagnetism
Publisher: American Geophysical Union (AGU)
Date: 06-1994
DOI: 10.1029/93TC03490
STARD for Abstracts: essential items for reporting diagnostic accuracy studies in journal or conference abstracts
Publisher: BMJ
Date: 17-08-2017
DOI: 10.1136/BMJ.J3751
Oxygen isotopes trace the origins of Earth's earliest continental crust
Publisher: Springer Science and Business Media LLC
Date: 31-03-2021
DOI: 10.1038/S41586-021-03337-1
Abstract: Much of the current volume of Earth's continental crust had formed by the end of the Archaean eon
Analysis of the Ragged Basin, Western Australia: Insights into syn-orogenic basin evolution within the Albany-Fraser Orogen
Publisher: Elsevier BV
Date: 05-2015
Early Proterozoic postcollisional granitoids of the Biryusa block of the Siberian craton
Publisher: GeoScienceWorld
Date: 07-2014
DOI: 10.1016/J.RGG.2014.06.002
Abstract: Comprehensive geochemical and geochronological studies were carried out for two-mica granites of the Biryusa block of the Siberian craton basement. U–Pb zircon dating of the granites yielded an age of 1874 ± 14 Ma. The rocks of the Biryusa massif correspond in chemical composition to normally alkaline and moderately alkaline high-alumina leucogranites. By mineral and petrogeochemical compositions, they are assigned to S-type granites. The low CaO/Na2O ratios (& .3), K2O ≈ 5 wt.%, CaO & 1 wt.%, and high Rb/Ba (0.7–1.9) and Rb/Sr (3.9–6.8) ratios indicate that the two-mica granites resulted from the melting of a metapelitic source (possibly, the Archean metasedimentary rocks of the Biryusa block, similar to the granites in εNd(t) value) in the absence of an additional fluid phase. The granite formation proceeded at 740-800 °C (zircon saturation temperature). The age of the S-type two-mica granites agrees with the estimated ages of I- and A-type granitoids present in the Biryusa block. Altogether, these granitoids form a magmatic belt stretching along the zone of junction of the Biryusa block with the Paleoproterozoic Urik–Iya terrane and Tunguska superterrane. The granitoids are high-temperature rocks, which evidences that they formed within a high-temperature collision structure. It is admitted that the intrusion of granitoids took place within the thickened crust in collision setting at the stage of postcollisional extension in the Paleoproterozoic. This geodynamic setting was the result of the unification of the Neoarchean Biryusa continental block, Paleoproterozoic Urik–Iya terrane, and Archean Tunguska superterrane into the Siberian craton.
Age and paleomagnetism of the 1210Ma Gnowangerup–Fraser dyke swarm, Western Australia, and implications for late Mesoproterozoic paleogeography
Publisher: Elsevier BV
Date: 06-2014
Geochemistry of the 755Ma Mundine Well dyke swarm, northwestern Australia: Part of a Neoproterozoic mantle superplume beneath Rodinia?
Publisher: Elsevier BV
Date: 04-2006
The Cambrian Carion Granite of Madagascar: A Case of Late Pan-African Shoshonitic Magmatism
Publisher: Elsevier BV
Date: 10-2001
Mafic intrusions in southwestern Siberia and implications for a Neoproterozoic connection with Laurentia
Publisher: Elsevier BV
Date: 07-2006
The evolution of a Precambrian arc-related granulite facies gold deposit: Evidence from the Glenburgh deposit, Western Australia
Publisher: Elsevier BV
Date: 03-2017
Rodinia connections between Australia and Laurentia: no SWEAT, no AUSWUS?
Publisher: Wiley
Date: 05-04-2002
Erratum to: Monazite trumps zircon: applying SHRIMP U–Pb geochronology to systematically evaluate emplacement ages of leucocratic, low-temperature granites in a complex Precambrian orogen (Contributions to Mineralogy and Petrology, (2017), 172, 8, (63), 10.1007/s00410-017-1386-5)
Publisher: Springer Science and Business Media LLC
Date: 16-08-2017
When will it end? Long-lived intracontinental reactivation in central Australia
Publisher: Elsevier BV
Date: 2019
A high-quality mid-Neoproterozoic paleomagnetic pole from South China, with implications for ice ages and the breakup configuration of Rodinia
Publisher: Elsevier BV
Date: 03-2000
Detrital zircon geochronology of the Speewah Group, Kimberley region, Western Australia: evidence for intracratonic development of the Paleoproterozoic Speewah Basin
Publisher: Informa UK Limited
Date: 03-04-2017
Petrology, geochronology, and tectonic implications of c . 500 Ma metamorphic and igneous rocks along the northern margin of the Central Asian Orogen (Olkhon terrane, La
Publisher: Geological Society of London
Date: 2008
Geochemistry and geochronology of the c. 1585Ma Benagerie Volcanic Suite, southern Australia: Relationship to the Gawler Range Volcanics and implications for the petrogenesis of a Mesoproterozoic sili
Publisher: Elsevier BV
Date: 06-2012
Radiogenic heating and craton-margin plate stresses as drivers for intraplate orogeny
Publisher: Wiley
Date: 04-05-2017
DOI: 10.1111/JMG.12249
The 1375Ma “Kibaran event” in Central Africa: Prominent emplacement of bimodal magmatism under extensional regime
Publisher: Elsevier BV
Date: 06-2010
Single-zircon geochronology and Nd isotopic systematics of Proterozoic high-grade rocks from the Mozambique belt of southern Tanzania (Masasi area): Implications for Gondwana assembly
Publisher: Geological Society of London
Date: 09-2003
Global record of 1600–700Ma Large Igneous Provinces (LIPs): Implications for the reconstruction of the proposed Nuna (Columbia) and Rodinia supercontinents
Publisher: Elsevier BV
Date: 2008
Age, geochemistry, and tectonic significance of Neoproterozoic alkaline granitoids in the northwestern margin of the Gyeonggi massif, South Korea
Publisher: Elsevier BV
Date: 10-04-2003
Proterozoic mafic magmatism in Siberian craton: An overview and implications for paleocontinental reconstruction
Publisher: Elsevier BV
Date: 12-2010
Cryogenian A-type Granites of the Yenisei Ridge – Indicators of Tectonic Transformation in the Southwestern Margin of the Siberian Craton
Publisher: GeoScienceWorld
Date: 06-2023
DOI: 10.2113/RGG20224532
Abstract: —We document the evolution of A-type granitoid magmatism during the Cryogenian tectonic transformation of the Yenisei Ridge from a postcollisional mode to the early stage of development of an active continental margin. We illustrate the A-type granitoid magmatism evolution in a model for the emplacement and cooling of the intrusions of the Strelka pluton, reflecting the final stage of magmatism during the formation of the postcollisional Glushikha complex (719–702 Ma). These processes took place at the same time as the formation of mantle, mantle-crustal and crustal rocks of the Tatarka complex (711–683 Ma), including the Yagodka pluton A-type granites (711–705 Ma) during the early stage of active continental margin development. During this period of tectonic transition, both convergent events involved the continuous formation of felsic intrusions corresponding to oxidized A-type granites.
Not-so-suspect terrane: Constraints on the crustal evolution of the Rudall Province
Publisher: Elsevier BV
Date: 09-2013
Age and palaeomagnetism of the Mundine Well dyke swarm, Western Australia: Implications for an Australia-Laurentia connection at 755 Ma
Publisher: Elsevier BV
Date: 03-2000
Age and Geochemical Characteristics of Major Mafic Dyke Swarms in the Southern Part of the Siberian Craton
Publisher: Wiley
Date: 10-2016
Paleomagnetism, geochronology and tectonic implications of the Cambrian-age Carion granite, Central Madagascar
Publisher: Elsevier BV
Date: 10-2001
Incremental pluton emplacement during inclined transpression
Publisher: Elsevier BV
Date: 06-2014
The role of multiple glacier outburst floods in proglacial landscape evolution: The 2010 Eyjafjallajokull eruption, Iceland
Publisher: Geological Society of America
Date: 30-07-2013
DOI: 10.1130/G34665.1
Evolution of the Queen Charlotte Basin: Further paleomagnetic evidence of Tertiary extension and tilting
Publisher: Elsevier BV
Date: 11-2000
Provenance of Neogene eolian red clay in the Altun region of western China—Insights from U Pb detrital zircon age data
Publisher: Elsevier BV
Date: 10-2016
Palaeomagnetic constraints on the position of the Kalahari craton in Rodinia
Publisher: Elsevier BV
Date: 08-2001
Structure and timing of Neoarchean gold mineralization in the Southern Cross district (Yilgarn Craton, Western Australia) suggest leading role of late Low-Ca I-type granite intrusions
Publisher: Elsevier BV
Date: 10-2014
Neoproterozoic tectonic structure of the Yenisei Ridge and formation of the western margin of the Siberian craton based on new geological, paleomagnetic, and geochronological data
Publisher: GeoScienceWorld
Date: 2016
DOI: 10.1016/J.RGG.2016.01.004
Abstract: There are continuing issues concerning the formation and reconstruction of the geographic position of the Neoproterozoic Yenisei Ridge—a key element of the western framing of the Siberian craton and the Central Asian orogenic belt. This study focuses on the inner structure, composition, and boundaries of the Central Angara terrane, which is the largest in the Transangarian segment of the Yenisei Ridge. We propose a scheme of fault deformation of the region and demonstrate that the fault tectonics of the Central Angara terrane is distinct from that of adjacent terranes. We study in detail the Yeruda pluton granitoids of the Teya complex, which indicate accretionary-collisional magmatic events in this terrane prior to its collision with Siberia. New geochemistry and SHRIMP U–Th–Pb zircon geochronology of the granites indicate that they formed at 880–860 Ma in a collisional setting. Integrated petromagnetic and paleomagnetic investigations yield a paleomagnetic pole that is significantly different from the corresponding Neoproterozoic interval of the apparent polar wander path (APWP) for Siberia. The difference in paleolatitudes between the Central Angara terrane and the Siberian craton at the time of the Teya granites formation was at least 8.6 degrees, which equals a latitudinal separation of at least 1000 km. We consider various possible positions for the terrane relative to the Siberian craton. These results demonstrate that the 880–860 Ma magmatic events in the Central Angara terrane are not related to events in the western margin of the Siberian craton. Therefore, they do not indicate the existence of a Grenville-age orogenic belt in this location, as proposed by some authors.
Two collisions, two sutures: Punctuated pre-1950Ma assembly of the West Australian Craton during the Ophthalmian and Glenburgh Orogenies
Publisher: Elsevier BV
Date: 09-2011
High-temperature granite magmatism, crust-mantle interaction and the mesoproterozoic intracontinental evolution of the Musgrave Province, Central Australia
Publisher: Oxford University Press (OUP)
Date: 07-04-2011
Constraints and deception in the isotopic record; The crustal evolution of the west Musgrave Province, central Australia
Publisher: Elsevier BV
Date: 03-2013
The 880–864Ma granites of the Yenisey Ridge, western Siberian margin: Geochemistry, SHRIMP geochronology, and tectonic implications
Publisher: Elsevier BV
Date: 04-2007
Archaean and Palaeoproterozoic gneisses reworked during a Neoproterozoic (Pan-African) high-grade event in the Mozambique belt of East Africa: Structural relationships and zircon ages from the Kidatu
Publisher: Elsevier BV
Date: 06-2006
Bioerosion: the other ocean acidification problem
Publisher: Oxford University Press (OUP)
Date: 08-03-2017
Abstract: Bioerosion of calcium carbonate is the natural counterpart of biogenic calcification. Both are affected by ocean acidification (OA). We summarize definitions and concepts in bioerosion research and knowledge in the context of OA, providing case ex les and meta-analyses. Chemically mediated bioerosion relies on energy demanding, biologically controlled undersaturation or acid regulation and increases with simulated OA, as does passive dissolution. Through substrate weakening both processes can indirectly enhance mechanical bioerosion, which is not directly affected by OA. The low attention and expert knowledge on bioerosion produced some ambiguous views and approaches, and limitations to experimental studies restricted opportunities to generalize. Comparability of various bioerosion and calcification rates remains difficult. Physiological responses of bioeroders or interactions of environmental factors are insufficiently studied. We stress the importance to foster and advance high quality bioerosion research as global trends suggest the following: (i) growing environmental change (eutrophication, coral mortality, OA) is expected to elevate bioerosion in the near future (ii) changes harmful to calcifiers may not be as severe for bioeroders (e.g. warming) and (iii) factors facilitating bioerosion often reduce calcification rates (e.g. OA). The combined result means that the natural process bioerosion has itself become a “stress factor”& #x94 for reef health and resilience.
Proterozoic crustal evolution of the Eucla basement, Australia: Implications for destruction of oceanic crust during emergence of Nuna
Publisher: Elsevier BV
Date: 05-2017
In situ SHRIMP U-Pb dating of monazite integrated with petrology and textures: Does bulk composition control whether monazite forms in low-Ca pelitic rocks during amphibolite facies metamorphism?
Publisher: Elsevier BV
Date: 06-2006
Warakurna large igneous province: A new Mesoproterozoic large igneous province in west-central Australia
Publisher: Geological Society of America
Date: 2004
DOI: 10.1130/G20171.1
Timing and Evolution of Cretaceous Island Arc Magmatism in Central Cuba: Implications for the History of Arc Systems in the Northwestern Caribbean
Publisher: University of Chicago Press
Date: 11-2011
DOI: 10.1086/662033
Late Mesoproterozoic (ca 1.2 Ga) palaeomagnetism of the Albany-Fraser orogen: No pre-Rodinia Australia-Laurentia connection
Publisher: Oxford University Press (OUP)
Date: 10-2003
Preserved intercratonic lithosphere reveals Proterozoic assembly of Australia
Publisher: Geological Society of America
Date: 02-08-2022
DOI: 10.1130/G50256.1
Abstract: The Proterozoic assembly of Australia, the understanding of which is critical for reconstructing Proterozoic supercontinents, involved amalgamation of the West Australian (WAC), North Australian (NAC), and South Australian cratons (SAC). However, the basement between these Archean to early Proterozoic lithospheric blocks is mostly buried beneath younger basins hence, its composition and age and the timing of Proterozoic assembly remain uncertain. In situ zircon U-Pb-O-Hf analyses of igneous rocks from drillholes that intersected basement beneath the northwestern Canning Basin reveal the presence of a substantial domain of juvenile Proterozoic lithosphere, the Percival Lakes province, between the WAC and NAC. Although isotopically distinct from the neighboring WAC and NAC, the Percival Lakes province is strikingly similar to other juvenile Proterozoic tectonic elements between the WAC, NAC, and SAC. Combining isotope and seismic data, we interpret the Percival Lakes province as part of an ~1700 × 400 km Proterozoic lithospheric domain that lacks evidence of Archean provenance but consists mainly of reworked remnants of Mesoproterozoic oceanic crust that survived WAC-NAC-SAC convergence. The apparent absence of Archean lithosphere between the cratons implies they never directly collided or that complete collision was prevented by impingement of three-dimensional promontories in the converging lithospheric blocks. Instead, the Percival Lakes province and other Proterozoic elements between the WAC, NAC, and SAC consist of oceanic lithosphere extracted from Earth's mantle in the Proterozoic. Our results imply that WAC-NAC convergence was younger than Columbia amalgamation at ca. 1.8 Ga and that Proterozoic Australia formed during the earliest phases of Rodinia assembly at ca. 1.3 Ga.
Isotopic constraints on stratigraphy in the central and eastern Yilgarn Craton, Western Australia
Publisher: Informa UK Limited
Date: 07-2012
Emplacement of the Argyle diamond deposit into an ancient rift zone triggered by supercontinent breakup
Publisher: Springer Science and Business Media LLC
Date: 19-09-2023
Ion microprobe U-Pb zircon and baddeleyite ages for the Great Dyke and its satellite dykes, Zimbabwe
Publisher: Geological Society of South Africa
Date: 03-2000
DOI: 10.2113/103.1.74
Cratonisation of Archaean continental crust: Insights from U–Pb zircon geochronology and geochemistry of granitic rocks in the Narryer Terrane, northwest Yilgarn Craton
Publisher: Elsevier BV
Date: 05-2022
Zircon geochronology of late archean komatiitic sills and their felsic country rocks, south-central Zimbabwe: A revised age for the reliance komatiitic event and its implications
Publisher: Elsevier BV
Date: 05-2013
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