ORCID Profile
0000-0001-7276-6273
Current Organisation
Yunnan University
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Inorganic Geochemistry | Geochemistry | Isotope Geochemistry | Tectonics
Expanding Knowledge in the Environmental Sciences | Expanding Knowledge in the Earth Sciences | Mineral Exploration not elsewhere classified |
Publisher: Elsevier BV
Date: 12-2012
Publisher: University of Chicago Press
Date: 09-2010
DOI: 10.1086/655113
Publisher: Elsevier BV
Date: 12-2012
Publisher: Geological Society of America
Date: 07-2011
DOI: 10.1130/G31991.1
Publisher: Elsevier BV
Date: 10-2010
Publisher: Informa UK Limited
Date: 23-05-2013
Publisher: Springer Science and Business Media LLC
Date: 09-2006
Publisher: Elsevier BV
Date: 12-2011
Publisher: Science China Press., Co. Ltd.
Date: 2004
DOI: 10.1360/03WD0624
Publisher: American Geophysical Union (AGU)
Date: 08-2019
DOI: 10.1029/2019JB017713
Publisher: IEEE
Date: 09-2017
Publisher: Geochemical Society of Japan
Date: 2006
Publisher: Elsevier BV
Date: 08-2013
Publisher: Royal Society of Chemistry (RSC)
Date: 2023
DOI: 10.1039/D3RA00603D
Abstract: Zn isotopic composition was firstly analyzed in twenty soil reference materials. A powerful new tool for tracing biochemical metal cycling at Earth's surface has been provided.
Publisher: Elsevier BV
Date: 02-2012
Publisher: Elsevier BV
Date: 2014
Publisher: Springer Science and Business Media LLC
Date: 04-06-2021
Publisher: Springer Science and Business Media LLC
Date: 08-08-2009
Publisher: Elsevier BV
Date: 10-2010
Publisher: Springer Science and Business Media LLC
Date: 29-08-2019
DOI: 10.1038/S41598-019-48988-3
Abstract: Illitic clay is ubiquitous in clastic hydrocarbon reservoirs, and the host for several radiometric isotopes such as the potassium-argon (K-Ar) and rubidium-strontium (Rb-Sr) systems. This study applied the isotope-dilution thermal ionization mass spectrometry technique for small s les (3–4 mg) to conduct illite Rb-Sr isotope dating of five illitic clay s les from the Silurian bituminous sandstone (SBS) intersected by five drillholes in the Tarim Basin, NW China. The 87 Rb/ 86 Sr ratio of clays is fractionated mainly by the addition of Rb during the illitization of mixed-layer illite/smectite (I/S), which is the dominant clay species in the Tarim Basin s les. The subs le-scale Rb/Sr isotope values suggest that each subs le may contain I/S particles of slightly variable degrees of illitization. Three of the analyzed s les (H6, KQ1 and TZ67) generated Rb-Sr isochron ages of 141 ± 61 Ma, 332 ± 32 Ma and 235 ± 8 Ma (errors quoted at 2σ), respectively. These results are similar to the corresponding K-Ar ages (125 Ma, 389 Ma and 234 Ma). The isotopic ages are consistent with the timing of hydrocarbon charge which varies in different drillholes as constrained by basin modelling, indicating that a closed-system behavior is attained by the hydrocarbon charge that inhibits the illitization of I/S. The Rb-Sr isotope analyses of the other two s les (YM35-1 and Q1) that did not yield isochron ages suggest the conditions for producing isochrons were not satisfied, which may be caused by disturbance of the isotope system by a post-charge hydrothermal event. The outcomes of this study show the robust potential of Rb-Sr clay subs le geochronology for cross-checking isotopic ages yielded by other systems (e.g. K-Ar system) and constraining the timing of hydrocarbon charge.
Publisher: Elsevier BV
Date: 10-2012
Publisher: Geological Society of America
Date: 11-2008
DOI: 10.1130/B26310.1
Publisher: Geological Society of America
Date: 2007
DOI: 10.1130/G23878A.1
Publisher: Elsevier BV
Date: 11-2004
Publisher: Elsevier BV
Date: 2010
Publisher: Springer Science and Business Media LLC
Date: 08-2005
DOI: 10.1360/03YD0265
Publisher: American Geophysical Union (AGU)
Date: 26-04-2022
DOI: 10.1029/2022GL098428
Abstract: Distinct signatures are present in the circum‐Pacific continental margins (e.g., kinematics, magmatism, and basin evolution), possibly influenced by the input of mid‐ocean ridge. It remains enigmatic why the circum‐Pacific continental margins that have experienced trench‐parallel mid‐ocean ridge subduction show erse geological evolution. Here we present geodynamic modeling results investigating trench‐parallel mid‐ocean ridge subduction and demonstrate two distinct types of model evolution. Type‐Ⅰ model includes a two‐stage steep subduction and is featured by slab detachment preceding the arrival of ridge at the trench. Type‐Ⅱ model is marked by a continuous flat subduction of mid‐ocean ridge with the opening of a slab window beneath intracontinental lithosphere. These two subduction styles produce erse tectono‐magmatic responses. Our results could explain the magmatic gap and forearc uplift during the Izanagi‐Pacific ridge subduction and the intraplate magmatic flare‐ups and tectonic uplift during the Nazca‐Antarctic ridge subduction, respectively.
Publisher: Elsevier BV
Date: 12-2012
Publisher: Elsevier BV
Date: 05-2012
Publisher: Springer Science and Business Media LLC
Date: 12-2004
DOI: 10.1038/NATURE03162
Abstract: Foundering of mafic lower continental crust into underlying convecting mantle has been proposed as one means to explain the unusually evolved chemical composition of Earth's continental crust, yet direct evidence of this process has been scarce. Here we report that Late Jurassic high-magnesium andesites, dacites and adakites (siliceous lavas with high strontium and low heavy-rare-earth element and yttrium contents) from the North China craton have chemical and petrographic features consistent with their origin as partial melts of eclogite that subsequently interacted with mantle peridotite. Similar features observed in adakites and some Archaean sodium-rich granitoids of the tonalite-trondhjemite-granodiorite series have been interpreted to result from interaction of slab melts with the mantle wedge. Unlike their arc-related counterparts, however, the Chinese magmas carry inherited Archaean zircons and have neodymium and strontium isotopic compositions overlapping those of eclogite xenoliths derived from the lower crust of the North China craton. Such features cannot be produced by crustal assimilation of slab melts, given the high Mg#, nickel and chromium contents of the lavas. We infer that the Chinese lavas derive from ancient mafic lower crust that foundered into the convecting mantle and subsequently melted and interacted with peridotite. We suggest that lower crustal foundering occurred within the North China craton during the Late Jurassic, and thus provides constraints on the timing of lithosphere removal beneath the North China craton.
Publisher: Elsevier BV
Date: 12-2018
Publisher: Elsevier BV
Date: 02-2014
Publisher: Elsevier BV
Date: 08-2016
Publisher: Elsevier BV
Date: 06-2009
Publisher: Springer Science and Business Media LLC
Date: 27-10-2020
Publisher: Elsevier BV
Date: 11-2013
Publisher: American Geophysical Union (AGU)
Date: 02-2019
DOI: 10.1029/2018JB016157
Publisher: Elsevier BV
Date: 06-2009
Publisher: Springer Science and Business Media LLC
Date: 10-2021
Publisher: Elsevier BV
Date: 05-2013
Publisher: Oxford University Press (OUP)
Date: 13-12-2012
Location: China
Start Date: 12-2014
End Date: 12-2018
Summary: Roles of deep-Earth fluid cycling in the generation of intra-continental magmatism. This project aims to test a provocative and potentially ground-breaking hypothesis that fluid released from subducted oceanic slabs and stored in the mantle transition zone, may trigger or control some major intra-plate geotectonic phenomena. It aims to provide a self-consistent model that links geological processes occurring at plate boundaries with those far-field effects well away from plate boundaries via dee .... Roles of deep-Earth fluid cycling in the generation of intra-continental magmatism. This project aims to test a provocative and potentially ground-breaking hypothesis that fluid released from subducted oceanic slabs and stored in the mantle transition zone, may trigger or control some major intra-plate geotectonic phenomena. It aims to provide a self-consistent model that links geological processes occurring at plate boundaries with those far-field effects well away from plate boundaries via deep-Earth fluid cycling. The outcomes of this project aim to help to better understand links between plume and plate tectonic processes in the first-order dynamic system of Earth, and identify ways to improve success in future mineral exploration. Read more Read less
Funder: Australian Research Council
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