The spatiotemporal variation in the altitudinal belts in the Kunlun Mountains reflects the natural geographical environment of the arid areas and is essential for constructing a dynamic change system of altitudinal belts in central and western China. In this study, we compiled the altitudinal belt spe...
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. ...
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...
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...
et al. Detrital-zircon geochronology and provenance of Ediacaran–Silurian rocks of the central to northern Tajikistan traverse: Geodynamic implications for the evolution of the Tian Shan. Gondwana Research, 2021, 99: 247-268. DOI:10.1016/j.gr.2021.07.013 79. Jia, Y., Glotzbach, C., Lixing...
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 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...
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, ...
Mass balance and a glacier surge of Guliya ice cap in the western Kunlun Shan between 2005 and 2015 2020, Remote Sensing of Environment Citation Excerpt : All the ICESat data re-measured were around 6000 m a.s.l., below the altitude (6200–6700 m a.s.l.) where ice cores were drille...