supported by the National Natural Science Foundation of China(Grant Nos.42250103 and 42174090);the Opening Fund of Key Laboratory of Geological Survey and Evaluation of Ministry of Education(Grant No.GLAB2023ZR02);the Ministry of Science and Technology(MOST)Special Fund from the State Key Laboratory of Geological Processes and Mineral Resources(Grant No.MSFGPMR2022-4)。
As a means of quantitative interpretation,forward calculations of the global lithospheric magnetic field in the Spherical Harmonic(SH)domain have been widely used to reveal geophysical,lithological,and geothermal vari...
supported by the National Natural Science Foundation of China(Nos.42174063,92155307,41976046);Guangdong Provincial Key Laboratory of Geophysical High-resolution Imaging Technology under(No.2022B1212010002);Project for introduced Talents Team of Southern Marine Science and Engineering Guangdong(Guangzhou)(No.GML2019ZD0203)。
Existing lithospheric velocity models exhibit similar structures typically associated with the first-order tectonic features,with dissimilarities due to different data and methods used in model generation.The quantifi...
supported by the National Natural Science Foundation of China(91958215);Shandong basic research office(WSR2023018);the Ministry of Education 111 Project(B18048)。
Evidence of seafloor spreading[1,2]proved the seafloor-spreading hypothesis[3]and led to the discovery of plate tectonics.A further observation-based analysis showed that seafloor-spreading results from downward pulli...
supported by the National Natural Science Foundation of China(Grant No.41730212);the Central Public-interest Scientific Institution Basal Research Fund(Grant No.2021IEF0103)。
As the western boundary of the Sichuan-Yunnan block(SYB),the Red River fault(RRF)is a major fault that controls deep crustal movement and deformation in the southeast margin of the Tibetan Plateau and regulates middle...
supported by the Geological Survey Project of the China Geological Survey for Regional Geophysical Survey in Beishan and Adjacent Areas(Grant No.DD20230254)。
1 Inctroduction The study of the earth's gravitational field is an important part of the explanation of the law of evolution and the distribution of materials on the earth.Gravity satellite is a new space exploration ...
supported by the National Natural Science Foundation of China(Grant No.42074092);the Youth Innovation Promotion Association of the Chinese Academy of Sciences(Grant No.2016064)。
The present-day lithospheric stress state of the Qinghai-Tibetan Plateau and neighboring areas is controlled by both the lithosphere itself and the underlying mantle.In other words,the stress is affected by the gravit...
supported by the Basic Scientific Fund for National Public Research Institutes of China(Grant No.2023S02);the National Natural Science Foundation of China(Grant Nos.42076076&42376075);the Taishan Scholar Program of Shandong Province。
Oceanic intraplate volcanoes with linear age progressions are usually accepted to be derived from melting of an upwelling mantle plume.Several seamount groups in NW Pacific,however,show complex age-distance relationsh...
Plume-lithosphere interactions are key in the coupling of deep Earth and surface processes,impacting deformation and evolution of sedimentary basins and continental topography at different spatial scales(Cloetingh et ...
supported by National Science Foundation of China(42102059 and 92055202);the China Geological Survey(DD20221817 and DD20190057);the basic scientific research funding in CAGS(J2204);the Second Tibetan Plateau Scientific Expedition and Research(2019QZKK0702).
Two suites of mafic dykes,T1193-A and T1194-A,outcrop in Gyangze area,southeast Tibet.They are in the area of Comei LIP and have indistinguishable field occurrences with two other dykes in Gyangze,T0902 dyke with 137....
supported by the National Natural Science Foundation of China(Grant Nos.41830212&42272243)。
1. Eclogites and the concept of viscous drainage Eclogites are a distinctive rock type, mainly composed of garnet and omphacite and formed through ultra-high-pressure metamorphism, wherein oceanic or continental crust...