ORCID Profile
0000-0003-2274-7933
Current Organisations
University of Melbourne
,
University of Adelaide
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Publisher: Springer Science and Business Media LLC
Date: 26-05-2023
DOI: 10.1038/S41598-023-35776-3
Abstract: Low-temperature thermochronology is a powerful tool for constraining the thermal evolution of rocks and minerals in relation to a breadth of tectonic, geodynamic, landscape evolution, and natural resource formation processes through deep time. However, complexities inherent to these analytical techniques can make interpreting the significance of results challenging, requiring them to be placed in their geological context in 4-dimensions (3D + time). We present a novel tool for the geospatial archival, analysis and dissemination of fission-track and (U-Th)/He data, built as an extension to the open-access AusGeochem platform ( ausgeochem.auscope.org.au ) and freely accessible to scientists from around the world. To demonstrate the power of the platform, three regional datasets from Kenya, Australia and the Red Sea are placed in their 4D geological, geochemical, and geographic contexts, revealing insights into the tectono-thermal evolutions of these areas. Beyond facilitating data interpretation, the archival of fission track and (U-Th)/He (meta-)data in relational schemas unlocks future potential for greater integration of thermochronology and numerical geoscience techniques. The power of formatting data to interface with external tools is demonstrated through the integration of GPlates Web Service with AusGeochem , enabling thermochronology data to be readily viewed in their paleogeographic context through deep time from within the platform.
Publisher: MDPI AG
Date: 24-01-2021
DOI: 10.3390/MIN11020116
Abstract: The Zhuguangshan complex hosts the main uranium production area in South China. We report (U-Th)/He and fission track thermochronological data from Triassic–Jurassic mineralized and non-mineralized granites and overlying Cambrian and Cretaceous sandstone units from the Lujing uranium ore field (LUOF) to constrain the upper crustal tectono-thermal evolution of the central Zhuguangshan complex. Two Cambrian sandstones yield reproducible zircon (U-Th)/He (ZHe) ages of 133–106 Ma and low effective uranium (eU) content (270–776 ppm). One Upper Cretaceous sandstone and seven Mesozoic granites are characterized by significant variability in ZHe ages (154–83 Ma and 167–36 Ma, respectively), which show a negative relationship with eU content (244–1098 ppm and 402–4615 ppm), suggesting that the observed age dispersion can be attributed to the effect of radiation damage accumulation on 4He diffusion. Correspondence between ZHe ages from sandstones and granites indicates that surrounding sedimentary rocks and igneous intrusions supplied sediment to the Cretaceous–Paleogene Fengzhou Basin lying adjacent to the LUOF. The concordance of apatite fission track (AFT) central ages (61–54 Ma) and unimodal distributions of confined track lengths of five s les from different rock units suggest that both sandstone and granite s les experienced a similar cooling history throughout the entire apatite partial annealing zone (~110–60 °C). Apatite (U-Th-Sm)/He (AHe) ages from six non-mineralized s les range from 67 to 19 Ma, with no apparent correlation to eU content (2–78 ppm). Thermal history modeling of data suggests that the LUOF experienced relatively rapid Early Cretaceous cooling. In most s les, this was followed by the latest Early Cretaceous–Late Cretaceous reheating and subsequent latest Late Cretaceous–Recent cooling to surface temperatures. This history is considered as a response to the transmission of far-field stresses, involving alternating periods of regional compression and extension, related to paleo-Pacific plate subduction and subsequent rollback followed by Late Paleogene–Recent India–Asia collision and associated uplift and eastward extrusion of the Tibetan Plateau. Thermal history models are consistent with the Fengzhou Basin having been significantly more extensive in the Late Cretaceous–Early Paleogene, covering much of the LUOF. Uranium ore bodies which may have formed prior to the Late Cretaceous may have been eroded by as much as ~1.2 to 4.8 km during the latest Late Cretaceous–Recent denudation.
Publisher: California Digital Library (CDL)
Date: 08-06-2023
DOI: 10.31223/X5SH3V
Abstract: Low-temperature thermochronology is a powerful tool for constraining the thermal evolution of geological materials at temperatures ( ~300 °C) common in the upper crust in relation to geodynamics, continental crustal evolution, landscape evolution, and natural resource formation and preservation. However, complexities inherent to these analytical techniques can make interpreting the significance of results challenging, requiring them to be placed in their geological context through time. We present a novel tool for the geospatial archival, analysis and dissemination of low-temperature thermochronology data (i.e., fission track and (U-Th)/He), built as an extension to the open-access AusGeochem platform (ausgeochem.auscope.org.au) and which is freely accessible to scientists from around the world. To demonstrate the power and utility of the platform, three regional low-temperature thermochronology datasets from Kenya, Australia and the Red Sea are presented. By visualising and interrogating these data in their regional three-dimensional geological, geochemical, and geographic contexts, insights into their tectonic implications are revealed which could otherwise be overlooked.
Publisher: Elsevier BV
Date: 09-2018
Publisher: Geological Society of America
Date: 12-08-2019
DOI: 10.1130/G46468.1
Abstract: The Turkana Depression of northern Kenya and southern Ethiopia contains voluminous plume-related basalts that mark the onset of the Paleogene–recent East African Rift System (EARS) at ca. 45 Ma. Thus, the Turkana Depression is crucial to understanding the inception of intracontinental rifting. However, the precise chronology of early rift-basin formation in Turkana is poorly constrained. We present apatite fission-track and (U-Th-Sm)/He thermochronology data from basement rocks from the margins of the north-south–trending Lokichar Basin that constrain the onset of rift-related cooling. Thermal history modeling of these data documents pronounced Eocene to Miocene denudational cooling of the basin-bounding Lokichar fault footwall. These results, along with ∼7 km of Paleogene to middle Miocene syn-rift strata preserved in the Lokichar fault hanging wall, suggest that formation of the Lokichar Basin began as early as ca. 45–40 Ma. Preexisting lithospheric heterogeneities inherited from earlier Mesozoic rifting and Eocene plume magmatism likely facilitated the broadly concurrent nucleation of strain in the Turkana Depression, up to ∼15 m.y. earlier than EARS initiation elsewhere. Late Paleogene extension in the Lokichar Basin and other parts of Turkana significantly predate the Miocene creation of pronounced plume-related topography in East Africa, suggesting that other mechanism(s), such as far-field stresses or mantle basal drag, likely played a critical role during EARS inception.
Publisher: Elsevier BV
Date: 11-2021
Publisher: American Geophysical Union (AGU)
Date: 03-2019
DOI: 10.1029/2018TC005210
Publisher: Copernicus GmbH
Date: 04-03-2021
DOI: 10.5194/EGUSPHERE-EGU21-10569
Abstract: & & The SciDataMover platform is a discipline- and scale-agnostic, lightweight, open source Data Movement Platform that transfers data, coupled with metadata from laboratories to shared workspaces then to repositories. The SciDataMover Platform leverages lightweight existing technologies that have a demonstrated capacity to be sustainably managed and can be affordably maintained.& & & & Despite significant investments in analytical instruments in Australian research laboratories relevant to earth sciences and particularly geochemistry, there has been underinvestment in storage and efficient, lossless transfer of data from & #8216 Private& #8217 lab instruments to & #8216 Collaboration& #8217 domains where researchers can analyse and share data, and then persist it to trusted & #8216 Publication& #8217 domains where researchers can persistently store the data that supports their scholarly publications.& & & & SciDataMover is a FAIR data movement platform that enables data from instruments to move in a scalable and sustainable manner and comprises:& & & & ) a data service to transfer data/metadata directly from instruments& br& ) collaboration areas to process, refine, standardise and share this data& br& ) a mechanism to transfer data supporting publications to a trusted repository (e.g., domain, institutional).& & & & The Platform, being built off existing components will enable researchers to have readily available access to laboratory data when and where they need it, along with the ability to collaborate with colleagues even during a pandemic where physical distancing is required. The benefits of SciDataMover are long term persistence of laboratory-generated data (at various stages from minimally processed to final published form), greater collaboration efficiency and enhanced scientific reproducibility.& &
Publisher: Copernicus GmbH
Date: 23-03-2020
DOI: 10.5194/EGUSPHERE-EGU2020-12452
Abstract: & & Low-temperature thermochronology has long been utilised in the Afro-Arabian Rift System (AARS) to examine exhumation cooling histories of normal fault footwalls and elucidate rifting chronologies where datable syn-rift strata and/or markers are absent. In particular, apatite fission track (AFT) and (U-Th)/He (AHe) analyses have constrained the timing and rate of rift-related, upper crustal thermal perturbations between ~30 and 120 & #176 C (up to ~5 km depth). In turn, these provide insights into the spatio-temporal evolution of in idual rift basins, morphotectonic rift shoulder development, normal fault system growth and, in some cases, the thermal influence of igneous intrusions and circulation of hot fluids. However, the relatively limited number of s les and confined areas generally involved in in idual case studies have precluded insights into longer wavelength tectonic and geodynamic phenomena, such as regional denudation trends and the growth of topography due to plume impingement.& & & & Here, we present a synthesis of & apatite fission track (AFT) and ~1000 (U-Th)/He (AHe) analyses from the Eocene-Recent AARS collated using LithoSurfer, a new cloud-based geoscience data platform. This continental-scale low-temperature thermochronology synthesis, the first of its kind in Africa, provides novel insights into the upper crustal evolution of the AARS that were previously difficult to decipher from an otherwise cumbersome and intractably large dataset. The data record a series of pronounced episodes of upper crustal cooling related to the development of the Red Sea, Gulf of Aden and East African Rift System (EARS). They also provide insights into the inherited tectono-thermal histories of these regions which controlled the spatial and temporal distribution of subsequent extensional strain.& & & & Thermochronology data trends along the AARS reflect a combination of rift maturity, structural geometry and geothermal regime, intrinsically linked to lithospheric architecture and magmatic activity. These relationships are best illustrated by contrasting the upper crustal thermal evolution of different AARS segments of varying age and complexity: for ex le, between the nascent Okavango, mature Ethiopian and evolved Red Sea rifts, wide (e.g. Turkana Depression) versus narrow (e.g. Main Ethiopian Rift) zones of deformation, between areas of transtensional (Dead Sea Transform), oblique (e.g. Gulf of Aden) and sub-orthogonal rifting (e.g. Malawi Rift), and the magmatic eastern versus amagmatic western branches of the EARS.& & & & A regional interpolation of standardised thermal history models generated from the mined AFT, AHe and, in some cases, vitrinite reflectance data yield Mesozoic-recent heat maps, extrapolated to produce paleo-denudation and burial histories for eastern Africa and Arabia. Integrating these thermotectonic images with other regional datasets allows for the interrelationship between tectonic and dynamic topography development, the denudation history of the land surface, and sediment transport and deposition to be explored in new ways.& & & & & & &
Publisher: Copernicus GmbH
Date: 04-03-2021
DOI: 10.5194/EGUSPHERE-EGU21-16550
Abstract: & & The AuScope Geochemistry Network (AGN) and partners Lithodat Pty Ltd are developing AusGeochem, a novel cloud-based platform for Australian-produced geochemistry data from around the globe. The open platform will allow laboratories to upload, archive, disseminate and publish their datasets, as well as perform statistical analyses and data synthesis within the context of large volumes of publicly funded geochemical data. As part of this endeavour, representatives from four Australian low-temperature thermochronology laboratories (University of Melbourne, University of Adelaide, Curtin University and University of Queensland) are advising the AGN and Lithodat on the development of low-temperature thermochronology (LTT)-specific data models for the relational AusGeochem database and its international counterpart, LithoSurfer. These schemas will facilitate the structured archiving of a wide variety of thermochronology data, enabling geoscientists to readily perform LTT Big Data analytics and gain new insights into the thermo-tectonic evolution of Earth& #8217 s crust.& & & & Adopting established international data reporting best practices, the LTT expert advisory group has designed database schemas for the fission track and (U-Th-Sm)/He methods, as well as for thermal history modelling results and metadata. In addition to recording the parameters required for LTT analyses, the schemas include fields for reference material results and error reporting, allowing AusGeochem users to independently perform QA/QC on data archived in the database. Development of scripts for the automated upload of data directly from analytical instruments into AusGeochem using its open-source Application Programming Interface are currently under way.& & & & The advent of a LTT relational database heralds the beginning of a new era of Big Data analytics in the field of low-temperature thermochronology. By methodically archiving detailed LTT (meta-)data in structured schemas, intractably large datasets comprising 1000s of analyses produced by numerous laboratories can be readily interrogated in new and powerful ways. These include rapid derivation of inter-data relationships, facilitating on-the-fly age computation, statistical analysis and data visualisation. With the detailed LTT data stored in relational schemas, measurements can then be re-calculated and re-modelled using user-defined constants and kinetic algorithms. This enables analyses determined using different parameters to be equated and compared across regional- to global scales.& & & & The development of this novel tool heralds the beginning of a new era of structured Big Data in the field of low-temperature thermochronology, improving laboratories& #8217 ability to manage and share their data in alignment with FAIR data principles while enabling analysts to readily interrogate intractably large datasets in new and powerful ways.& &
Publisher: American Chemical Society (ACS)
Date: 08-2023
Publisher: Frontiers Media SA
Date: 12-07-2021
DOI: 10.3389/FEART.2021.713448
Abstract: The Oligocene-Recent Red Sea rift is one of the preeminent ex les of lithospheric rupture in the recent geological past, forming the basis for many models of how continental breakup occurs and progresses to the formation of new oceanic crust. Utilisation of low-temperature thermochronology in the Red Sea Rift since the 1980s has been key to constraining its spatio-temporal evolution, providing constraints for the propagation of strain and geomorphological development of its margins where datable syn-tectonic strata and/or markers are absent. We review the wealth of published apatite fission track and (U-Th-Sm)/He data from along the Red Sea, affording insights into the Oligocene-Recent thermo-tectonic evolution of the Nubian and Arabian margins. A regional interpolation protocol was employed to synthesise time-temperature reconstructions generated from the mined thermochronology data and burial histories produced from vitrinite reflectance and well data. These cooling-heating maps record a series of pronounced episodes of upper crustal thermal flux related to the development of the Oligocene-Recent Red Sea Rift. Assimilation of these regional thermal history maps with paleogeographic reconstructions and regional magmatic and strain histories provide regional perspectives on the roles of tectonism and geodynamic activity in Red Sea formation and their effects on rift margin development.
Publisher: Copernicus GmbH
Date: 28-03-2022
DOI: 10.5194/EGUSPHERE-EGU22-12874
Abstract: & & One of the greatest challenges in the global geochemistry community is to aggregate and make the large amounts of geochemical data generated by laboratories FAIR [Findable, Accessible, Interoperable, and Reusable] and publicly available the large amounts of data generated in laboratories. Standardisation and data organisation has often been an in idual or voluntary/uncoordinated effort and/or motivated by the likelihood of immediate/near-future publication. Along with the technical challenges of getting laboratory data into a well-structured relational database and linked to s les& #8217 metadata, societal and cultural issues are often present around the standardisation and accessibility of data reporting (e.g. equipment manufacturer, funding body proprietary data outputs, data reduction software accessibility and requirements/& #8220 data ownership& #8221 of the users/scientists).& & & & & & & & & In response to a national expression of a need to address the challenges outlined above and for better organisation and coordination of Australian geochemistry laboratories and data, AuScope funded the AuScope Geochemistry Network (AGN) in 2019. The AGN comprises a team of researchers, data-scientists, and technical staff from three universities across Australia Curtin University, the University of Melbourne, and Macquarie University, tasked in coordinating and strategizing the best approach to:& & & ul& & li& Unite the erse Australian geochemistry community.& /li& & li& Promote national capability (existing geochemical capability).& /li& & li& Promote investment in infrastructure (new, advanced geochemical infrastructure).& /li& & li& Support increased end user access to laboratory facilities.& /li& & li& Support professional development via online tools, training courses and workshops.& /li& & li& Preserving legacy data sets& /li& & /ul& & & & & & & & Over the last two years the AGN has worked to organise the geochemistry community and provide solutions to the integration and adoption of international best practices for data management. With the & #8216 end in mind& #8217 the AGN and collaborator Lithodat have developed the AusGeochem platform, a unique research data platform that services laboratory needs, bridges the gap between s le metadata and analytical data as well as strengthens the user-laboratory connection. To establish data reporting tables that fit the community& #8217 s need, yet facilitate FAIR data practices and integrating international best practices for handling geochemistry data, the AGN led and coordinated Expert Advisory Groups composed of geochemical specialists from a number of Australian institutions. Along with the AusGeochem platform that allows laboratories to upload, archive, disseminate and publish their datasets the AGN has built LabFinder, a web application tool that helps geoscience users find and access the right laboratory and analytical technique to solve their research questions. LabFinder aims to continue to support end user access to laboratory facilities leading to the improvement in the capability and capacity of geochemistry laboratories on a national scale. In the coming two years AGN will continue to build upon these accomplishments by expanding the AGN data partnerships through the on boarding of institutions hosting major geochemistry laboratories, further facilitating collaborations between Australian geochemistry laboratories.& &
Publisher: American Geophysical Union (AGU)
Date: 2018
DOI: 10.1002/2017TC004575
Publisher: American Geophysical Union (AGU)
Date: 08-2022
DOI: 10.1029/2022GC010390
Abstract: Northern Malawi's Nyika Plateau is a 3,700 km 2 large, highly elevated (∼2,500 m) plateau located at the western margin of the Miocene‐Recent Malawi rift and the confluence of multiple Proterozoic orogenic belts. Neighboring asthenospheric upwelling in the Rungwe Volcanic Province, associated with the active East African Rift, has created similar topographic highs, leading some to speculate that the formation of Nyika could be related. Here, we present new low‐temperature data using apatite fission track, apatite (U‐Th‐Sm)/He and zircon (U‐Th)/He thermochronology to constrain the upper crustal thermal history of the Nyika region since the Devonian. The data suggest that Nyika was an isolated feature since at least the Permo‐Triassic, well before more recent rifting in Malawi, and may have developed as a horst between two large Karoo grabens, the Henga‐Ruhuhu and the North Rukuru to the southeast and northwest, respectively. Similarities between the thermal histories of Nyika and the currently separated Livingstone Plateau to the east allow for the possibility that these may have been connected in a contiguous highland prior to the formation of the intervening Neogene Malawi rift. Thermal history models for exposed Precambrian basement s les adjacent to Nyika, and once buried beneath the neighboring Karoo basins, indicate that up to 3.4 km of Permo‐Triassic section has since been eroded, with s les along the plateau not indicating burial of Karoo‐type sediment at this time. Most recent cooling histories suggest that the plateau surface continued to denude at varying degrees from the Cretaceous and reached near‐surface temperatures in the Late Paleogene‐Neogene.
Publisher: Copernicus GmbH
Date: 23-03-2020
DOI: 10.5194/EGUSPHERE-EGU2020-22432
Abstract: & & AuScope is an Australian consortium of Earth Science institutes cooperating to develop national research infrastructure. AuScope received federal funding in 2019 to establish the AuScope Geochemistry Laboratory Network (AGN), with the objective of coordinating FAIR-based open data initiatives, support user access to laboratory facilities, and strengthen analytical capability on a national scale.& & & & & Activities underway include an assessment of best practices for researchers to register s les using the International Geo S le Number (IGSN) system in combination with prescribed minima for meta-data collection. Initial activities will focus on testing meta-data schema on high value datasets such as geochronology (SHRIMP U-Pb, Curtin University), geochemistry (Hf-isotopes, Macquarie University) and low-temperature thermochronology analyses (fission track/U-He, University of Melbourne). Collectively, these datasets will lead to a geochemical data repository in the form of an Isotopic Atlas eResearch Platform that is available to the public via the AuScope Discovery Portal. Over time, the repository will aggregate a large volume of publicly funded geochemical data, providing a key resource in quantitatively understanding the evolution of Earth system processes that have shaped the Australian continent and its resources.& &
Publisher: American Geophysical Union (AGU)
Date: 27-09-2021
DOI: 10.1029/2021EO163702
Abstract: Brutal university cuts are putting at risk an industry crucial to addressing climate change Down Under and around the world. Saving geoscience will require a community reckoning.
Publisher: Copernicus GmbH
Date: 04-03-2021
DOI: 10.5194/EGUSPHERE-EGU21-14628
Abstract: & & The AuScope Geochemistry Network (AGN, www.auscope.org.au/agn) was established in 2019 in response to a community expressed desire for closer collaboration and coordination of activities between Australian geochemistry laboratories. Its aims include: i) promotion of capital and operational investments in new, advanced geochemical infrastructure (ii) supporting increased end user access to laboratory facilities and research data (iii) fostering collaboration and professional development via online tools, training courses and workshops. Over the last six months, the AGN has coordinated a monthly webinar series to engage the geoscience community, promote FAIR data practices and foster new collaborations. These webinars were recorded for future use and can be found at: hannel/UC0zzzc6_mrJEEdCS_G4HYgg.& & & & A primary goal of the AGN is to make the networks& #8217 laboratory geochemistry data, from around the globe, discoverable and accessible via development of an online data platform called AusGeochem (www.auscope.org.au/ausgeochem). Geochemical data models for SHRIMP U-Pb, Fission Track, U-Th/He, LA-ICP-MS U-Pb/Lu-Hf and Ar-Ar are being developed using international best practice and are informed by expert advisory groups consisting of members from various institutes and laboratories within Australia. AusGeochem is being designed to provide an online data service for analytical laboratories and researchers where s le and analytical data can be uploaded (privately) for processing, synthesis and secure dissemination to collaborators. Researcher data can be retained in a private space but studied within the context of other publicly available data. Researchers can also generate unique international geo s le numbers (IGSNs) for their s les via a build in link to the Australian Research Data Commons IGSN registry.& & & & & AusGeochem supports FAIR data practices by providing researchers with the ability to include links to their AusGeochem registered data in research publications, providing a potential opportunity for AusGeochem to become a trusted data repository.& &
Publisher: Informa UK Limited
Date: 02-04-2016
Publisher: American Geophysical Union (AGU)
Date: 04-2023
DOI: 10.1029/2022JB024358
Abstract: The fast‐slipping Alpine (∼30 mm/yr), Hope (∼10–20 mm/yr) and Kelly (∼6 mm/yr) faults in the South Island of New Zealand form a complex intersection zone that accommodates tectonic strain along the Australian‐Pacific plate boundary. Analysis of digital topography reveals evidence for stream capture, drainage ide migration, landscape responses to incipient fault development, and preserved enclaves of relic topography that collectively reflect complex interplays between active faulting and landscape evolution. (U‐Th)/He thermochronology of zircon (ZHe) and apatite (AHe) is used to investigate the low‐temperature thermal evolution of rocks in the intersection zone. Weighted mean s le ages for ZHe single grain ages ( n = 13 s les) range from ∼9 to 2 Ma, and AHe multi‐grain and single grain aliquot ages ( n = 9 s les) range from ∼1.5 to 0.5 Ma. Inverse and forward thermal history modeling reveals distinct spatiotemporal variations in thermal histories. Late Miocene exhumation rates (∼0.6–3.5 km/Myr, assuming geothermal gradients of 33–40 °C/km) through crustal depths of approximately 5–6 km, are interpreted to be controlled by proximity to the Alpine fault, with rocks proximal to the fault recording faster exhumation rates relative to distal s les. Establishment of the Hope‐Kelly fault system in the Quaternary structurally juxtaposed rocks with discordant cooling histories. Rocks throughout the study region record increased cooling rates from ∼2 Ma. Possible causal mechanisms include, spatial changes in rock uplift associated with transport toward the Alpine Fault, increased erosion rates associated with Quaternary climate change, or increased rock mass erodibility associated with development of the Hope‐Kelly fault system.
Publisher: Copernicus GmbH
Date: 28-03-2022
DOI: 10.5194/EGUSPHERE-EGU22-13429
Abstract: & & Over the last two years, the Australian AuScope Geochemistry Network (AGN) has developed AusGeochem in collaboration with geoscience-data-solutions company Lithodat Pty Ltd. This open, cloud-based data platform (ausgeochem.auscope.org.au) serves as a geo-s le registry, with IGSN minting capability, a geochemical data repository and a data analysis tool. With guidance from experts in the field of geochemistry from a number of Australian institutions, and following international standards and best practices, various s le and geochemistry data models were developed that align with the FAIR data principles. AusGeochem is currently accepting data of SIMS U-Pb as well as of fission track and (U-Th-Sm)/He techniques with LA-ICPS-MS U-Pb and Lu-Hf, & sup& & /sup& Ar/& sup& & /sup& Ar data models under development. Special attention is paid to the implementation of streamlined workflows for AGN laboratories to facilitate ease of data upload from analytical sessions. Analytical results can then be shared with users through AusGeochem and where required can be kept fully confidential and under embargo for specified periods of time. Once the analytical data on in idual s les are finalized, the data can then be made more widely accessible, and where required can be combined into specific datasets that support publications.& &
Publisher: Elsevier BV
Date: 10-2018
No related grants have been discovered for Samuel C Boone.