Figure 2. The sketch geological map of the mafic-ultramafic intrusions in Xiwanggou area 1-Quaternary; 2-Dacite member of Upper Triassic Elashan Formation; 3-Gneiss member of Paleoproterozoic Baishahe Formation; 4-Early Jurassic syenogranite; 5-Middle Triassic monzonitic granite; 6-Late Ordovic...
a-Division of tectonic units in the western Kunlun orogenic belt; b-Geological sketch map of Maeryang a: TRMB-Tarim plate; WKLS-western Kunlun orogenic belt; KKLS-Karakorun orogenic belt; TSHT-Tianshuihai terrane; BYF-Bayankela faultfolded belt; SQT- Qiangtang terrane; F1- Kongur- Kegang...
et al. Discovery of the Ordovician arc‑type gabbros in Nanpingxueshan area, West Kunlun orogenic belt, and its geological significance | [西昆仑南屏雪山地区奥陶纪弧型辉长岩 的发现及其地质意义]. Scientia Geologica Sinica, 2024, 59(1): 82-102. DOI:10.12017/dzkx.2024.006 37. Tao, Z., ...
Discovery of Kunlunshan-type rock glaciers and the classification of rock glaciers. Chin. Sci. Bull. 30 Z3., 365-369 ZKexue Tongbao..Zhijiu, C. (1985), Discovery of Kunlunshan-type rock glaciers and the classification of rock glaciers, Kexue Tongbao, 30 (3), 365-369.Cui Zhijiu....
c Geological map of Weidong showing the location of pyroxene diorite Full size image In spite of the spatial variations of mineralization, the orebodies in the Weibao deposit are all hosted by the Mesoproterozoic Langyashan Formation that predominantly consists of limestone, marble, skarn, schist, ...
The East Kunlun region is located east of the Erla Mountains, extending west to the Qinghai-Xinjiang border, north to the Qaidam Basin and south to the Muzitage-Buqing Shan line (Fig. 1). It stretches nearly 1000 km from east to west and has a north–south extent of 100–210 km. Th...
One is between the Upper Permian Gequ Formation and the underlying Upper Carboniferous Haoteluowa Formation, and the other lies between the Upper Triassic Elashan (Babaoshan) Formation and the underlying Lower to Middle Triassic Hongshuichuan Formation. The former was considered as a continental ...
The northern part of the western Kunlun (southern margin of the Tarim basin) represents a Sinian rifted margin. To the south of this margin, the Sinian to Paleozoic Proto-Tethys Ocean formed. South-directed subduction of this ocean, beneath the continental southern Kunlun block during the Paleozo...
Wang Guocan, Zhang Tianping, Liang Bin, Cheng Nengsong, Zhu Yunhai, Zhu Jie, Bai Yongshan. 1999. Composite ophiolite melange zone in central part of eastern eection of eastern Kunlun orogenic zone and geological significance of "Fault belt in central part of eastern section of eastren Kunlun...
Fig. 1. Geological sketch map of the Altyn–Qilian–North Qaidam orogenic system in the northern Qinghai-Tibet Plateau (modified from Zhang JX et al., 2015). CAOB–Central Asian Orogenic Belt; NQL–North Qilian subduction-accretion complex belt; QLB–Qilian Block; NQD–North Qaidam subduction-...