ORCID Profile
0000-0002-8575-3516
Current Organisations
University of Tokyo
,
Geological Survey of Western Australia
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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.
Geology | Geochronology | Environmentally sustainable engineering | Inorganic geochemistry | Basin Analysis | Stratigraphy (incl. Biostratigraphy and Sequence Stratigraphy) | Sedimentology | Geochemistry | Isotope Geochemistry
Oil and Gas Exploration | Mining and Extraction of Energy Resources not elsewhere classified | Expanding Knowledge in the Earth Sciences | Mineral Exploration not elsewhere classified | Primary Mining and Extraction of Mineral Resources not elsewhere classified |
Publisher: Elsevier BV
Date: 12-2015
Publisher: Geological Society of London
Date: 2011
DOI: 10.1144/M36.67
Publisher: Petroleum Exploration Society of Australia (PESA)
Date: 30-08-2022
DOI: 10.36404/JNNB3567
Abstract: The Oodjuongari Structure (-16.636, 134.205), seen on aeromagnetic data as a circular feature (Figures 2, 3a and 5), and traversed by four 2D seismic reflection profiles (Figures 6 and 7), is interpreted as a possible impact crater concealed by superficial Cainozoic strata. There is no surface expression of the structure which is located within the Beetaloo Sub-basin and overlying Georgina Basin, although small streams appear to deviate around the feature (Figure 3b). The structure appears to be circular on the aeromagnetic data and has a maximum diameter of 5 km. It has similar size and aeromagnetic signature to the Foelsche impact structure located 275 km to the east (Haines & Rawlings, 2002). In both cases the pronounced circular aeromagnetic feature appears to be related to a circular disruption of flat-lying mafic volcanics, which are the Mid-Cambrian Antrim Plateau Volcanics at Oodjuongari. If the Oodjuongari Structure is an impact structure, the 5 km diameter would be consistent with a complex crater with a central uplift.
Publisher: Wiley
Date: 02-2002
Publisher: Geological Society of America
Date: 06-2014
DOI: 10.1130/G35434.1
Publisher: American Geophysical Union (AGU)
Date: 08-2019
DOI: 10.1029/2019JB017713
Publisher: Informa UK Limited
Date: 09-2005
Publisher: Informa UK Limited
Date: 19-05-2009
Publisher: Elsevier BV
Date: 2010
Publisher: MDPI AG
Date: 28-03-2023
DOI: 10.3390/NU15071649
Abstract: Glucose is a vital fuel for fetal growth, and carbohydrates are the primary source of glucose in the diet. The effects of carbohydrate intake during pregnancy on neonatal birth weight have not been fully investigated or systematically reviewed. Therefore, this systematic review aimed to collate the available evidence to determine whether carbohydrate intake during pregnancy impacts newborn birth weight. A literature search was performed from inception to March 2022 in Embase, Medline, and PsycInfo. Articles published in English were independently screened for the title and abstracts, and then for full texts. Out of 17 studies included, a significant relationship between the intake of maternal carbohydrate or its subcomponents and neonatal birth weight was reported in six studies. Of them, one study reported that higher carbohydrate intake in early pregnancy was associated with lower birth weight. The two other studies reported a positive correlation between maternal carbohydrate intake and neonatal birth weight regarding first- and second-trimester intake. Maternal carbohydrate intake may have an impact on birth weight, as suggested by the included studies in this systematic review. However, the overall review indicates contradictory findings concerning the relationship between carbohydrate intake and neonatal birth weight. Studies assessing the type of carbohydrate and the amount consumed with improved methodological quality are recommended.
Publisher: Informa UK Limited
Date: 06-2007
Publisher: Informa UK Limited
Date: 09-2005
Publisher: Geological Society of America
Date: 15-04-2019
DOI: 10.1130/G45915.1
Publisher: Informa UK Limited
Date: 03-1989
Publisher: Informa UK Limited
Date: 04-11-2015
Publisher: Wiley
Date: 11-06-2019
DOI: 10.1111/MAPS.13307
Publisher: Informa UK Limited
Date: 12-2006
Publisher: SEPM (Society for Sedimentary Geology)
Date: 08-09-2017
Publisher: Informa UK Limited
Date: 12-1987
Publisher: Geological Society of America
Date: 18-07-2019
DOI: 10.1130/G38000.1
Publisher: Informa UK Limited
Date: 09-2005
Publisher: Informa UK Limited
Date: 07-2013
Publisher: Informa UK Limited
Date: 12-2001
Publisher: Elsevier BV
Date: 11-2004
Publisher: American Association of Petroleum Geologists AAPG/Datapages
Date: 04-2017
Publisher: Elsevier BV
Date: 11-2015
Publisher: University of Chicago Press
Date: 09-2009
DOI: 10.1086/600866
Publisher: Elsevier BV
Date: 06-2014
Publisher: Elsevier BV
Date: 2015
Publisher: SEPM (Society for Sedimentary Geology)
Date: 08-09-2017
Publisher: Informa UK Limited
Date: 06-2003
Publisher: SEPM (Society for Sedimentary Geology)
Date: 08-09-2017
Publisher: Informa UK Limited
Date: 12-2009
Publisher: Elsevier BV
Date: 07-2020
Publisher: Elsevier BV
Date: 08-1988
Publisher: Informa UK Limited
Date: 08-1998
Publisher: Informa UK Limited
Date: 08-1998
Publisher: Elsevier BV
Date: 08-2007
Publisher: Elsevier BV
Date: 08-2004
Publisher: Elsevier BV
Date: 12-2015
Publisher: Elsevier BV
Date: 10-2001
Publisher: Elsevier BV
Date: 09-2015
Publisher: Informa UK Limited
Date: 04-2008
Publisher: Informa UK Limited
Date: 1998
Publisher: Geological Society of London
Date: 05-1998
Publisher: Elsevier BV
Date: 03-2000
Publisher: CSIRO Publishing
Date: 2021
DOI: 10.1071/AJ20038
Abstract: Barnicarndy 1 is a stratigraphic well drilled in the southern part of the Canning Basin’s Barnicarndy Graben under Geoscience Australia’s Exploring for the Future program in collaboration with the Geological Survey of Western Australia to provide stratigraphic data for this poorly understood tectonic component. The well intersects a thin Cenozoic section, Permian–Carboniferous fluvial clastics and glacial diamictites and a thick pre-Carboniferous succession (855–2585mRT) unconformably overlying Neoproterozoic metasedimentary rocks. Three informal siliciclastic intervals were defined based on core lithology, well logs, chemical and mineral compositions: the Upper Sandstone (855–1348.1mRT), Middle Interval (1348.1–2443.4mRT) and Lower Sandstone (2443.4–2585mRT). The Middle Interval was further ided into six internal zones. Both conventional methods and artificial neural network technology were applied to well logs to interpret petrophysical and elastic properties, total organic carbon (TOC) content, pyrolysis products from the cracking of organic matter (S2) and mineral compositions. Average sandstone porosity and reservoir permeability are 17.9% and 464.5mD in the Upper Sandstone and 6.75% and 10mD in the Lower Sandstone. The Middle Interval claystone has an average porosity and permeability of 4.17% and 0.006mD, and average TOC content and S2 value of 0.17wt% and 0.047mgHC/g rock, with maximum values of 0.66wt% and 0.46mgHC/g rock, respectively. Correlations of mineral compositions and petrophysical, geomechanical and organic geochemical properties of the Middle Interval have been conducted and demonstrate that these sediments are organically lean and lie within the oil and gas window.
Publisher: Wiley
Date: 10-2003
Publisher: CSIRO Publishing
Date: 2010
DOI: 10.1071/AJ09026
Abstract: Reassessment of stratigraphic relationships and biostratigraphic data pertaining to the Carribuddy Group and Worral Formation in all relevant petroleum wells and many mineral drill holes across the southern Canning Basin has led to the following important results. The Carribuddy Group is restricted to the Late Ordovician to earliest Silurian. The overlying Worral Formation is mostly of Silurian age and does not intertongue with the Middle Devonian Tandalgoo Formation, as previously thought. A thin basin-wide chronostratigraphic marker—the Pegasus Dolomite Member (previously referred to as dolomite spike or dolomite marker) of the Sahara Formation—allows improved correlation between salt-bearing sub-basins and adjacent condensed Carribuddy Group successions. The Mallowa Salt is not as extensive as previously thought rather the Minjoo Salt thickens to become the only salt seal in the eastern and southern Kidson Sub-basin. The Carribuddy Group forms the regional seal to the prospective Larapintine 2 petroleum system, but also contains local source and reservoir facies. The Bongabinni Formation contains extremely rich oil-prone source rocks in local lagoonal facies along the Admiral Bay Fault Zone these rocks have been linked by other studies to migrated oil in that area. The distribution of the source facies is poorly known, but it may extend down-dip into more mature parts of the Willara Sub-basin, and west into offshore areas. Other local source units may be present in the Mallowa Salt, and possibly the Nibil Formation, but are not well documented. Aeolian sandstone with excellent reservoir potential is locally present in the Nibil Formation, but is more extensive in the lower Worral Formation, particularly the Elsa Sandstone Member.
Publisher: Informa UK Limited
Date: 2002
Publisher: CSIRO Publishing
Date: 2021
DOI: 10.1071/AJ20160
Abstract: Funded by Geoscience Australia’s Exploring for the Future initiative and operated by the Geological Survey of Western Australia, the Waukarlycarly 1 deep stratigraphic drillhole was designed to investigate the geology of the little-known Waukarlycarly Embayment and assess the petroleum, mineral, groundwater and CO2 storage potential of the area. Based on consultation with the Western Desert Lands Aboriginal Corporation on the cultural significance of the name, Waukarlycarly, it has been agreed to change the name of the well to Barnicarndy 1 and the tectonic sub ision to the Barnicarndy Graben. This and all future publications will now refer to the Barnicarndy 1 stratigraphic drillhole (previously Waukarlycarly 1) and the Barnicarndy Graben (previously Waukarlycarly Embayment). Drilling commenced on 1 September 2019 and reached a total depth (TD) of 2680.53m on 30 November 2019, recovering more than 2km of continuous core. The cored interval extended from 580m to TD in Neoproterozoic Yeneena Basin dolostone, which was unconformably overlain by a thick, lower Canning Basin Ordovician stratigraphy, including richly fossiliferous marine mudstones with common volcanic ash beds. A major unconformity is located at the top of the Ordovician section where it is overlain by sandstones and muddy diamictites of the Carboniferous–Permian Grant Group, followed by a Cenozoic succession near surface. Ditch cuttings were collected from surface to 580m at 3m intervals. The pre-Grant Group Paleozoic succession is unique within the Canning Basin, indicating that the Barnicarndy Graben’s depositional history is markedly different when compared with adjacent structural sub isions, such as the Munro Arch and Kidson Sub-basin. Detrital zircon geochronology, biostratigraphy and borehole imaging interpretation assisted in the definition of two new geological units within the Ordovician stratigraphy of Barnicarndy 1: the Yapukarninjarra and Barnicarndy formations. Preliminary routine core analysis data indicates the potential for CO2 storage within the Barnicarndy Formation beneath a Grant Group seal. The well also provides new insights into the structural interpretation of the Barnicarndy Graben.
Publisher: Informa UK Limited
Date: 09-2005
Publisher: Informa UK Limited
Date: 06-2001
Publisher: Informa UK Limited
Date: 1991
Publisher: Elsevier BV
Date: 07-2015
Publisher: CSIRO Publishing
Date: 2001
DOI: 10.1071/SB97028
Abstract: Silicified leaf impressions attributed to the tribe Banksieae (Proteaceae) are reported from a new Tertiary macroflora from near Glen Helen, Northern Territory and from the Miocene Stuart Creek macroflora, northern South Australia. The fossil leaf material is described and placed in Banksieaeformis Hill & Christophel. Banksieaeformis serratus sp. nov. is very similar in gross morphology to the extant Banksia baueri R.Br. and B. serrata L.f. and is therefore representative of a leaf type in Banksia that is widespread geographically and climatically within Australia and that is unknown in Dryandra or other genera of the Banksieae. The leaf material from Stuart Creek and Woomera represents the lobed leaf form typical of Paleogene macrofloras from southern Australia, but one species,B. langii sp. nov., is closely similar in gross form to Banksieaephyllum taylorii R.J.Carpenter, G.J.Jordan & R.S.Hill et al. from the Late Paleocene of New South Wales and similarly may be sclerophyllous. Also reported are impressions of Banksia infructescences, or ‘seed cones’, in Neogene sediments near Marree and Woomera, South Australia. These fossils demonstrate the presence of Banksiinae in central Australia in the mid-Tertiary, potentially indicating the former existence of linking corridors between now widely separated populations of Banksia.
Start Date: 07-2019
End Date: 06-2022
Amount: $352,000.00
Funder: Australian Research Council
View Funded ActivityStart Date: 09-2023
End Date: 09-2026
Amount: $612,689.00
Funder: Australian Research Council
View Funded ActivityStart Date: 06-2023
End Date: 06-2026
Amount: $405,000.00
Funder: Australian Research Council
View Funded Activity