jointly supported by the National Natural Science Foundation of China (No.41890831);China Postdoctoral Science Foundation (No.2022M712571);MOST Special Fund from the State Key Laboratory of Continental Dynamics,Northwest University。
The provenance and tectonic implications of Late Paleozoic sedimentary rocks in the South Qinling Belt(SQB) provide important clues for understanding the timing and mechanism of the collision between North China Block...
supported by the National Natural Science Foundation of China(Nos.41572002,41830320,and 41661134047)。
Focusing on the Shuixiakou Section(Xikou area,Zhen’an County,Shaanxi Province,southeastern Qinling region,China),the Roadian-Wordian conodonts are investigated.More than 2000 conodont elements including 6 genera and ...
supported by the National Natural Science Foundation of China(Nos.41830320,45172002,41661134047)。
Based on a study of 49 conodont and 57 geochemical samples from the Upper Triassic,carbonate-dominated Dengdengqiao Formation,Qinling Basin,China,the Carnian conodonts and carbon isotope records are first reported.Two...
the Project of the Youth Science and Technology New Star in Shaanxi Province(No.2017KJXX-94);the National Natural Science Foundation of China(Nos.41102037,41421002);the Project of Investigation and Evaluation of Uranium Resources(No.DD2016013623);the National Excellent Doctoral Dissertation of China(No.201324)。
Paleozoic granites can provide important insights of crustal differentiation and collision process of the North Qinling terrane. The Dafanggou leucogranites that intruded in the Qinling Complex is a Paleozoic granite ...
supported by the National Natural Science Foundation of China (Nos. 41350110224, 41750110483, 41730426, 41872066);the Open Research Project of the State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (No. GPMR201820)
Ophiolites play a key role in understanding subduction-accretion-collision processes. Herein, we discuss origin and metamorphic evolution of an enigmatic, Neoproterozoic ophiolite candidate—the mafic-ultramafic Songs...
financially supported by the National Natural Science Foundation of China (No. 41672064);the International Geoscience Programme “Diamonds and Recycled Mantle” (No. IGCP-649)
The Songshugou peridotite massif is located in the north of Shangdan suture zone, North Qinling orogenic belt of Central China. The massif is mainly composed of fine-grained mylonitic dunites, coarse-grained dunites, ...
supported by the China Geological Survey (Nos. DD20190358, 20190370 and 20190448);the National Natural Science Foundation of China (No. 41472172)
The Qinling Complex from the Qinling orogenic belt was generally considered to be part of the Caledonian orogeny, however information of the Grenville event of the Qinling Complex has been poorly recognized. Two grani...
the National Natural Science Foundation of China(Nos.41530211,41502046);the China Geological Survey(No.DD20160030);The Fundamental Research Funds for the Central Universities,China University of Geosciences(Wuhan)(No.CUGCJ1711)is also acknowledged for partial financially support
The Wulong diorite porphyry displays a very unusual flower-like glomerophyric texture and is thus well-known as a gemstone type of "Luoyang peony stone" for non-geologists. Hereby, we present a comprehensive study i...
supported by the "Strategic Priority ResearchProgram" of the Chinese Academy of Sciences (No.XDB03020402);the National Basic Research Program (973) of China (No. 2013CB956403);the National Natural Science Foundation of China (Nos. 41201005, 41272128);the Funda-mental Research Funds for the Central Universities (No.lzujbky-2013-122);the NSFC National Innovative ResearchTeam Project (No. 41021091)
The western Qinling (秦岭) orogenic belt is one of the outermost ranges in the northeas- tern Tibetan Plateau. Its tectonic uplift history is therefore essential to insight on the evolution history of the plateau. H...
supported by the Special Research Project of the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences (No. 1008);the National Natural Science Foundation of China (No. 90714008)
Two types of melt pockets, closed melt pocket (CMP) and open melt pocket (OMP), are recognized from the peridotite xenoliths entrained in the Cenozoic kamafugites in western Qinling (秦岭), Central China. The Ha...