financially supported by the Fundamental Scientific Research Project of Institute of Geology,China Earthquake Administration(Grant No.IGCEA2016);the National Natural Science Foundation of China(Grant Nos.42204072 and 41804055);the National Key Research and Development Program of China(Grant No.2017YFC1500103)。
The Ordos Block,the western part of the North China Craton(NCC),has preserved most of its cratonic lithospheric roots during the destruction and modification of the NCC,and nowconnects two distinctly different tectoni...
supported by National Natural Science Foundation of China (Grant Nos. 40672080 and 40921062);"111" Project (Grant No. B08030);Excellent Youth Teacher Fund of China University of Geosciences (Wuhan)
The Laojunshan Formation is a suite of molasse formed during the rapid uplift of the North Qilian Orogenic Belt (NQOB). Forty-one samples of sandstone have been collected from the Sunan and Minle sections in the weste...
Sponsored by the National Natural Science Foundation of China (Grant Nos. 40672080 and 40621002);the Developing Plan of Innovation Group of Ministry of Education of China (Grant No. IRT0546)
The Caledonian North Qilian orogenic belt lies between the North China plate and the Qaidam mi-croplates, and resulted from the collision among the Qaidam microplate, mid-Qilian block and the North China plate. The or...
supported by the National Natural Science Foundation of China(Grant No.40534052).
In order to explore the disputed issue concerning the tectonic affinity ofthe ancient ocean mantle of North Qilian Mountains (NQM), geochemical and Sr, Nd, Pb isotopiccompositions of pillow basalts of the Yushigou Oph...
the National KeyBasic Research Development Project of China(Grant No.19980408);the Key Project of Knowledge Innovation of the CAs(Grant No.KZcx2-314); the National Key Project of Science and Technology(Grant No.2001-BA611B-O1).
Using seven well-replicated Qilian juniper (Sabina przewalskii Kom.) ring-width chronologies developed at Zongwulong and Shalike Mts. in the northeastern part of the Qaidam Basin annual precipitation from previous Jul...
the NSFC(Grant No.40334038,40121303);the National Key Project for Basic Research on the Tibetan Plateau(Grant No.G1998040809);CAS"Hundred Talents Project"(Grant No.Ren-Jiao-Zi[2000]02821.
Cenozoic sediments in the foreland basin--Jiuquan Basin in west Hexi Corridor recorded tectonic uplift information of the Qilian Mountains. High resolution paleomagnetic dating of the Laojunmiao (LJM) section across t...
supported by the Major Knowiedge Innovation Project of the Chinese Aademy of Sciences(Gant Nos.KZCX1-1002 and KZCX1-1009);the opening fund of the Key Laboratory of Ice-core and Cold-regions Environment,Cold and Arid Regions Environment and Engineering Research Insti tute,Chinese Academy ofSciences(Grant No.210506)..
Based on the cross-dated tree-ring samples collected from the middle Qilian Moun- tain, a standard ring-width chronology had been developed, which covered the period AD 1000 to 2000. The correlations between the chron...
This project was funded by the National Natural Science Foundation of China (Grant Nos. 49925410 and 40102021).
Lower Cretaceous red sedimentary rocks from the depositional basin of East Qilian fold belt have been collected for a paleomagnetic study. Stepwise thermal demagnetization reveals two or three components of magnetizat...
Proterozoic volcanic rocks of the western part from the North Qilian Mountains are the products of continental rift volcanism, belonging to continental flood basalts, the petrogeochemistry of which apears to suggest t...
There are three groups of pillow volcanics in the Dachadaban ophiolite. Group 1 is typical boninite, enriched in Si, Mg and depleted in Ti, HREE and HFSE; group 2 is the evolved boninite, slightly higher abundance of ...