Supported by the National Natural Science Foundation of China(Nos.42322302,42373048);the Youth Innovation Promotion Association,Chinese Academy of Sciences(No.2022207);the Strategic Priority Research Program of the Chinese Academy of Sciences(No.XDB42020303);the Laoshan Laboratory(No.LSKJ202204100)。
Marine carbonates,the major carrier of carbon upon the upper crust,can be subducted into the Earth’s interior along with oceanic crust,and then returned to the surface through magmatism,which constitute the deep carb...
funded by the National Natural Science Foundation of China(41773052,41973058)。
Due to their high density,the ilmenite-bearing cumulates(IBC)(with or without KREEP)formed during the late-stage lunar magma ocean solidification are thought to sink into the underlying lunar mantle and trigger lunar ...
supported by the National Natural Science Foundation of China(42074112,4171101169,41574086,41274095 and 42374110);the Central Publicinterest Scientific Institution Basal Research Fund(JKYZD202302 and JKY202221);the Geological Investigation Project(DD20230008 and DD20221643);the DFG Deutsche Forschungsgemeinschaft(392149212);supported by the‘CUG Scholar’Scientific Research Funds at China University of Geosciences(Wuhan)(2022114);the Sino-German(CSC-DAAD)Postdoc Scholarship.
The mechanism that causes the rapid uplift and active magmatism of the Hoh-Xil Basin in the northern Tibetan Plateau and hence the outward growth of the proto-plateau is highly debated,more specifically,over the relat...
South of Godé, in the central-western region of Burkina Faso, granitoids of Paleoproterozoic age are similar to those of the Man/Leo shield. This study focused on the petrographic and geochemical characteristics of t...
The Pouni area is made up of basalts belonging to the Boromo belt, lamprophyres and granitoids. These geological formations are similar to geological formations of the same type in other regions of the Palaeoproterozo...
financially supported by the Ministry of Sciences and Technology of China(Grant No.2022YFF0800901);the Natural Science Foundation of China(Grant Nos.92055206 and 42163007)。
Cenozoic potassic-ultrapotassic igneous rocks are widespread in the southeastern Tibetan Plateau.Their petrogenesis and magmatic processes remain subject to debate in spite of numerous publications.Almost all of the C...
supported by National Key R&D Program of China(2022YFF0800902);National Natural Science Foundation of China(No.42121002);the Open Research Project from the State Key Laboratory for Mineral Deposits Research,Nanjing University(2022-LAMD-K11);SinoProbe Lab 202204,State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences(GPMR202110);the 111 Project(B18048);the Fundamental Research Funds for the Central Universities(2-9-2019-034).
Recent studies have shown that Cu-rich sulfide accumulates in the lower continental crust and serves as a critical reservoir to balance Cu depletion in the upper crust.Recycling of Cu in the lower crust is also assume...
substantially supported by the National Nature Science Foundation of China(Grant No.41872220)。
The North Qinling Orogenic Belt(NQOB)is a composite orogenic belt in central China.It started evolving during the Meso-Neoproterozoic period and underwent multiple stages of plate subduction and collision before enter...
sponsored by the National Key R&D Programme of China(2021YFC2901803);National Natural Science Foundation of China(92055314 and 41802095);the China Geological Survey(DD20230049 and DD20220983);is a contribution to the International Geoscience Programme(IGCP-741);Academician Bao-jun Liu Foundation of Southwest Geological Science and Technology Innovation Center.
The Cenozoic Himalayan leucogranite-pegmatite belt has been a hotspot for rare metal exploration in recent years.To determine the genesis of the pegmatite in the Himalayan region and its relationship with the Greater ...
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...