The spatial variation of Asian dust and marine aerosol contributions to glaciochemical signals in central Asia [PDF]
Short-term (6 months to 17 years) glaciochemical records have been collected from several glacier basins in the mountains of central Asia. The spatial distribution of snow chemistry in central Asia is controlled by the influx of dust from the large ...
Mayewski, Paul A, Wake, Cameron P
core +1 more source
Ultra-deep oil and gas structure is the key field of exploration and development in the southern margin of Junggar Basin. In this area, the formation lithology is complex, the rock strength is high, and the drilling engineering has problems such as low ...
Yang Hu +6 more
doaj +1 more source
The boundary between the Central Asian Orogenic belt and Tethyan tectonic domain deduced from Pb isotopic data [PDF]
Castillo, Paterno R +7 more
core +1 more source
Discovery of ∼4.0 Ga detrital zircons in the Aermantai ophiolitic mélange, East Junggar, northwest China [PDF]
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Stable Isotopic Constraints of the Turpan Basin in Northwestern China [PDF]
Stable isotopic analysis of sedimentary rocks can be used to reconstruct past geologic changes in the elevation and climate of topographic features such as mountain ranges and plateaus. The Tibetan Plateau is an ideal field laboratory for conducting this
Schaen, Allen J.
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Objective Multiple types of oil reservoirs, including conventional oil, tight oil, and shale oil, have been discovered from the slope area to the depression area in the Jimusaer Depression, demonstrating the characteristics of conventional ...
ZHI Dongming +5 more
doaj +1 more source
Background Xinjiang serves as an important coal production base in northwestern China. This region holds approximately 40% of China’s predicted coal reserves, with its coal resources primarily distributed in coal-accumulating basins such as Junggar, Yili,
Shuzheng NING +7 more
doaj +1 more source
Tectonic evolution of the northern part of Western Tianshan (Xinjiang, NW China).
The Yili Block is important for understanding the Late Paleozoic geodynamic evolution of Central Asia. It is bounded to the north by the Northern Tianshan Carboniferous flysch and ophiolitic mélange.
Charvet, Jacques +4 more
core +1 more source
Lithospheric structure across the Himalayan-Tibetan orogen: a petrological and geophysical study [PDF]
HKT-ISTP 2013 ...
Fernàndez, M. +2 more
core
Single-Factor Comprehensive Reservoir Quality Classification Evaluation-Taking the Hala'alat Mountains at the Northwestern Margin of the Junggar Basin as an Example. [PDF]
Pu Q +10 more
europepmc +1 more source

