supported by the National Natural Science Foundation of China(Grants Nos.42372074,42030307,41972058 and 41802056);Natural Science Basic Research Program of Shaanxi(Program Nos.2023-JC-QN-0366 and 2023-JC-YB-254);the MOST Special Fund from the State Key Laboratory of Continental Dynamics.
Existing studies provide adequate petrological evidences on ca.500 Ma ultra-high pressure(UHP)metamorphism in the North Qinling Orogenic Belt(NQOB)in central China,but the genesis of 470-420 Ma multi-phase granulite-f...
supported by funds from the Strategy Priority Research Program(Category B)of Chinese Academy of Sciences(XDB0710000);the National Natural Science Foundation of China(42103037,42373046);the Fundamental Research Funds for the Central Universities.
Extreme fractionation of elements and isotopes in mafic igneous rocks is abnormal in deciphering the source nature and melting conditions of mafic magmatism.Especially,identification of geochemically ultra-depleted ma...
financially supported by the National Natural Science Foundation of China(No.41972198);the Science and Technology Innovation Program of Hunan Province(No.2021RC4055);the Cooperation Foundation of Key Laboratory of Mineralogy and Metallogeny,Guangzhou Institute of Geochemistry;CAS(No.KLMM20180201);the Scientific Research Starting Foundation of Central South University。
In order to decipher element mobility in UHP meta-sedimentary rocks in the continental subduction zone,major and trace element compositions are investigated for a continuous profile from a representative UHP region in...
funded by two Second Tibetan Plateau Comprehensive Scientific Investigation and Research Projects(2019QZKK0702,2019QZKK0706);a project of National Natural Science Foundation of China(42230311);two geological survey projects of China Geological Survey(DD20221635,DD20221811).
As one of the important Paleo-Tethys suture zones in eastern Tibet,the Jinshajiang orogenic belt is of great significance to study the tectonic evolution of the main suture zone of Paleo-Tethys.In this paper,eclogites...
supported by the Strategic Priority Research Program(B)of the Chinese Academy of Sciences(Grant No.XDB41000000);the National Key R&D Program of China(Grant No.2018YFA0702703);the National Natural Science Foundation of China(Grant Nos.41925017,41721002);the Fundamental Research Funds for the Central Universities(Grant No.WK2080000144)。
The X-discontinuity is characterized by 2–8% wave impedance contrasts and indistinguishable seismological Clapeyron slopes. Its origin is not yet entirely understood and attributed to a variety of plausible causes, a...
supported by the National Science Foundation of China(Grant Nos.92055202);the Second Tibetan Plateau Scientific Expedition and Research(Grant No.2019QZKK0702);the China Geological Survey(Grant Nos.DD20221817 and DD20221630)。
The formation of titanite coronae after rutile is common in retrograde high-to ultrahigh-pressure meta-mafic rocks,which provides a good opportunity to address the geochemical behavior of HFSE in crustal environments....
financially supported by the National Key Research and Development Program of China(Grant No.2019YFA0708501);the National Natural Science Foundation of China(Grant No.42172060)。
Natural gas,consisting primarily of methane(CH_(4)),has become a major source of clean energy in modern society in many parts of the globe.Recent experimental observations and discoveries of deep-sourced abiotic CH_(4...
supported by the National Key Research and Development Program of China(2019YFA0708501);the National Natural Science Foundation of China(42172060 and 41702052)。
Methane(CH_(4))is a critical but overlooked component in the study of the deep carbon cycle.Abiotic CH_(4)produced by serpentinization of ultramafic rocks has received extensive attention,but its formation and flux in...
funded by the Grant Agency of the Czech Republic(GACR)project 19-25035S to P.Štípskáand the International Partnership Program of CAS 773(132744KYSB20190039)to Y.Jiang;Institutional supports of the Research Project no.310760(Strategic Research Plan of the Czech Geological Survey-DKRVO/CGS 2018-2022);Centre for Geosphere Dynamics(UNCE/SCI/006)of Faculty of Sciences,Charles University
Mid-Devonian high-pressure(HP)and high-temperature(HT)metamorphism represents an enigmatic early phase in the evolution of the Variscan Orogeny.Within the Bohemian Massif this metamorphism is recorded mostly in alloch...
The absence of ultrahigh pressure(UHP)orogenic eclogite in the geological record older than c.0.6 Ga is problematic for evidence of subduction having begun on Earth during the Archean(4.0-2.5 Ga).Many eclogites in Pha...