This work was supported by the National Key Research and Development Program of China(2018YFC0604002);the Geological Survey program of China Geological Survey(DD20221643-6);the Fundamental Research Funds of Chinese Academy of Geological Sciences(JKY21021,JKY202122).
The magma source,petrogenesis,tectonic setting and geochronology of the late Paleozoic A-type granites widely exposed in the Zhaheba area,East Junggar,have thus far not been well-constrained.A better understanding of ...
financially supported by funds of the Second Tibetan Plateau Scientific Expedition and Research Program(2019QZKK0801);the National Key R&D Program of China(Grant Nos.2021YFC2901704)。
The Tianyu Cu-Ni sulfide deposit occurs in the north margin of the Central Tianshan Arc in East Tianshan orogenic belt, Xinjiang, NW China. The intrusions consist of gabbro, peridotite, and olivine pyroxenite. The per...
financially supported by Deep Resources Exploration and Mining Project(Grant No.2019YFC0605202);Chinese Geological Survey(Grant No.DD20221684)。
The Early-Middle Devonian Shugouzi Formation in the Quruqtagh block consists mainly of clastic rocks.However,their provenance has been scarcely studied since it was named.Geochemistry of clastic rocks was commonly use...
jointly funded by the special project of the fundamental scientific research of the Institute of Geology, China Earthquake Administration (Grant No. IGCEA2121);the National Natural Science Foundation of China (Grant No. 41572331, 41272386)。
Objective Betula microphylla Bunge, as a resource treasury of desert biodiversity, is a pioneer plant in saline-alkaline soil amelioration. According to previous research, Ebinur Lake, north Xinjiang, is a representat...
supported by the National Natural Science Foundation of China(Grant No.40830420,41702097,41972092)。
Objective Lop Nur is one of the world’s largest Quaternary salt lakes and is currently a playa. In this lake, unique giant glauberite deposits occur, of which the intercrystalline pores host super-large liquid potash...
the National Natural Science Foundation of China (Grant #41872003)
Two Upper Devonian to Lower Carboniferous sections,namely the Bulongguoer and Haer(Gennaren area)in the Junggar Basin,Central Asian Orogenic Belt,in northwestern China were examined with regard to ichnology and palyno...
This research was funded by the National Science Foundation for Young Scientists of China(No.41602176);Key Laboratory of Tectonics and Petroleum Resources(TPR–2018–16).
During the Late Paleozoic,West Junggar(Xinjiang,NW China)experienced a shift in tectonic setting from compression to extension.Ha'erjiao is an important area for investigating collisional structures,post–collisional ...
granted by Petro China Innovation Foundation(Grant No.2019D-5007-0214);the National Mega Project of Oil and Gas(Grant No.2017ZX05013005-009)。
The micro-nano pore structure of conglomerate in the Lower Karamay Formation of the Xinjiang Oilfield,Junggar Basin,northern China is characterized to predict its impact on fluid reserves and seepage.Authigenic clay m...
financially supported by the National Nature Science Foundation of China(grant No.41572057);National 305 Project(grant No.2011BAB06B01-03)。
Objective The Xiemisitai area,located in the northern part of West Junggar,Xinjiang,is the eastern extension of the Boshchekul-Chingiz volcanic arc in China,which is characterized by a large number of Paleozoic volcan...
financially supported by Ministry of Science and Technology(No.2015CB453004);China National Nuclear Corporation(No.LTD1612-4)。
The Mengqiguer deposit in the southern Yili basin Ili Basin is a large interlayer-oxidation-zone type uranium deposit.In this paper,we applied multiple methods including microscopic observation,scanning electron micro...