supported by the National Natural Science Foundation of China(Nos.U22B6002,42422402,41902202 and 42276222);the SINOPEC Key Laboratory of Geophysics(No.FW0399-0029);the Second Tibetan Plateau Scientific Expedition and Research(No.2019QZKK00708);the Development Fund of South China Sea Institute of Oceanology of the Chinese Academy of Sciences(No.SCSIO202207);the Special Fund of the Institute of Geophysics,China Earthquake Administration(No.DQJB22B23)。
The boundary between cratonic and orogenic lithospheres is a significant seismogenic zones marked by intense lithospheric deformation.The Sichuan Craton(SCC),as a key tectonic block bordering eastern Tibetan Plateau,r...
supported by the DREAM project of the National Key R&D Program of China(No.2016YFC0600402);the National Natural Science Foundation of China(No.41774071);the US Gelogical Survey Earthquake Hazards Program。
We present crustal models for seismic P-waves(Vp),S-waves(Vs)and the Vp/Vs ratio across the southern North China Craton along latitude 36°N.Our results are based on inverse and forward modeling of long-range wide-ang...
support of the CAPES and the Brazilian National Research Council (CNPq) for the Doctoral (No. 140411/2013-5)。
The Gentio metagranitoid presents equigranular and porphyritic facies, modal composition ranging from tonalite to monzogranite with calculated T_(Zr)<800 ℃ for most samples. Its mineralogy is dominated by quartz and ...
This study was supported by the National Natural Science Foundation of China(Nos.41802240,41902036);the Fundamental Research Funds of the Central Universities granted by China University of Geosciences(Wuhan)(No.007-G1323541792)to Hao Deng;This research was also supported by an opening fund from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(Wuhan)(No.GRMR201607).
The chrome spinel(chromite)in mantle peridotites from ophiolites can shed light on the formation and evolution process of ophiolites.Podiform chromites were found in the Late Proterozoic Miaowan ophiolitic complex(MOC...
supported by funds from the NSFC/NRF Research Cooperation Programme (No. 41761144061);the NSFSD (No. ZR2016DM04);the SDUST Research Fund (No. 2015TDJH101)
Pelitic granulite from the Huangtuyao area,occurrs in the Huai'an Complex,is located in the Trans-North China Orogen of the North China Craton.On the basis of petrolography,mineral component,and phase equilibrium mode...
supported by the National Natural Science Foundation of China (No. 41761144061);the Shandong Provincial Natural Science Foundation (No. ZR2016DM04);the University Students Innovation Program of SDUST (No. 2015TDJH101)
The studied mafic granulites are located at Xiwangshan,Xuanhua region in the north of the Trans-North China Orogen(TNCO),occurring as lens within tonalite-trondhjemite-granodiorite(TTG)gneisses in the eastern part of ...
financially supported by the National Key Research and the Development Program of China (No. 2016YFC0600502);the National Natural Science Foundation of China (No. 41502046);the Geological Survey Project of China (No. DD20160030)
Coronitic microstructures have been used to interpret the late-stage solidification history of igneous rocks and to constrain the corresponding chemical and/or physical changes. Coronas with three shells were also rec...
supported by the National Natural Science Foundation of China(No.41602234);the Fundamental Research Funds for the Central Universities,China University of Geosciences,Wuhan,China(Nos.CUGL180406,CUGCJ1707);Open Fund(No.GRMR201901)from the State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan
Electron probe microanalysis(EPMA) dating of monazite has been developed over decades. However, limited by the detectability and analytical sensitivity of dating-related elements(Th, Pb, U and Y), the EPMA dating has ...
supported by the MOST Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (No. MSFGPMR16);the Key Program of the Ministry of Land and Resources of China (No. 1212011220497)
Archean high-K granitoids, generally formed after tonalite-trondhjemite-granodiorite (TTGs), are important for understanding crustal reworking of ancient cratons. The Linshan Archean high-K granitoids from the souther...
financially supported by the Nation Key R&D Program of China (No. 2017YFC0601305-01);the China Geological Survey (Nos. DD20160048-04, DD2016034308, DD20160343-09)
The Bainaimiao Group, which crops out in the Sonid Right Banner area of Inner Mongolia, China, comprises mainly metamorphosed volcano-sedimentary rocks. This group can be divided into two formations: a lower formation...