supported by the National Natural Science Foundation of China(Grant Nos.42030306,42372263&41972206);the Center for Deep-Time Digital Earth Frontier Science(Grant No.2652023001)。
The NE-striking Longmen Shan thrust belt(LSTB)in the eastern margin of the Tibetan Plateau is located at the junction of the Songpan-Ganze Terrane and the Yangtze block.This belt experienced the Late Triassic Qinling-...
the financial support from the UGC CAS-I & II grant;DSTs New Delhi for financial assistance to MJ. BPD
The chemical and petrological correlation of metamorphic nappes and klippes overlying the Proterozoic sedimentary units in the Kumaun Himalaya is still debated. The Ramgarh and Almora gneisses, not previously distingu...
the National Natural Science Foundation of China (Grant Nos. 41372028, 41225009 & 41472193);the Project of Major State Special Research on Petroleum (Grant No. 2011ZX05008-001)
The Longmenshan thrust belt(LMTB) is one of the best natural laboratories for thin-skinned tectonics and has developed a series of NE-SW trending fold-and-thrust structures represented by a series of nappes and klippe...
The Nampula Subprovince in Northern Mozambique is a Mesoproterozoic gneiss terrane with a Pan-African(523-550 Ma)amphibolite-facies met- amorphic overprint.The province forms a pivotal part of the evolution and final ...
The arcuate nappe structure on the north edge of the Wuliang Mountains in westernYunnan Province is a complex nappe structural system with multiple superimposed structures.The autochthonous system is a WNW-trending ar...
Project supported by the National Natural Science Foundation of China.
There are many Sinian-Cambrian (Z^c-∈_b) epimetamorphic blocks either in groups or scatteredly covering the granitoids in the area of Guangning-Zhaoqing, the northwestern part of Wuchuan-Sihui faults in western Guang...
An enormous thrust nappe and a metamorphic core complex of extensional origin have been recently discovered within the Hercynian-Indosinian orogen of Inner Mongolia. Both features are of the Mesozoic age, but the form...