1-D P- and S-wave velocity models for the collision zone between the northern Tianshan mountain and the Junggar basin based on local earthquake data [PDF]
We have developed crustal minimum 1-D P- and S-wave velocity models of the collision zone between the northern Tianshan mountain and the Junggar basin (86°E–89°E, 43°N–44.5°N).
Sun, Anhui +3 more
core +1 more source
Terrestrial heat flow in Junggar Basin, Northwest China
Based on temperature logs of 117 boreholes and thermal conductivity of 119 rock samples, the first group of 35 heat flow data in the Junggar Basin are presented. The thermal gradients vary between 11.6 and 26.5°C/km, and the thermal conductivity changes from 0.17 to 3.6 W/mK. Heat flow ranges from 23.4 to 53.7 mw/m2 with a mean of (42.3±7.7) mW/m2. The
Shejiao Wang +4 more
openaire +1 more source
The chemical and isotopic compositions of the natural gas and the co-produced flowback water from the XJC 1 well in Junggar Basin, China, were analyzed to determine the origin of gases in the Permian Lucaogou Formation (P2l) and the Triassic Karamay ...
Lin Zhang +5 more
doaj +1 more source
The Seismic Sedimentology Application Research on Junggar Basin
Depending on different seismic frequencies and reflection interface information of sedimentary bodies, the core technologies involved in sedimentology had been introduced into clastic transpressional basins developing in Junggar Basin in the ways of the macro (seismic geomorphology) and micro (seismic lithology) to design a data interpretation process ...
Chuanchun Song +3 more
openaire +2 more sources
The Mesozoic palaeorelief of the northern Tian Shan (China) [PDF]
International audienceThe Tian Shan range offers a natural laboratory to study orogenic processes. Most of the previous studies focused on either the Palaeozoic evolution of the range or its Cenozoic intracontinental evolution linked with the India-Asia ...
Augier, Romain +6 more
core +3 more sources
Junggar basin, northwest China: trapped Late Paleozoic ocean
Abstract The Junggar basin originated during the late Paleozoic as either a remnant lower to mid-Paleozoic ocean basin or a mid-Carboniferous back-arc (intra- or inter-arc) basin bounded by emergent volcanic arcs south of the Siberian Craton. The retreating Junggar Sea left behind a regressive sedimentary section comprising at least 3–4 km of marine ...
Alan R. Carroll +6 more
openaire +1 more source
Modern Southern Junggar Foreland Basin System Adjacent to the Northern Tian Shan, Northwestern China
Building-up of the modern Tian Shan range due to the India-Eurasia collision induces the flexural subsidence of the southern Junggar block. The sedimentary infill and subsidence in the southern Junggar foreland basin recorded the growth of the northern ...
Chao Li +9 more
doaj +1 more source
Stable isotope characterization of pedogenic and lacustrine carbonates from the Chinese Tian Shan: constraints on the Mesozoic - Lower Cenozoic palaeo-environmental evolution [PDF]
International audienceIn the Mesozoic–Cenozoic continental deposits of the Tian Shan area, two main levels containing pedogenic carbonates have been identified on both the southern and northern foothills of the range: one in the Upper Jurassic series and
Barrier, Laurie +8 more
core +4 more sources
Altaids in the Central Asian Orogenic Belt (CAOB) is one of the world’s largest orogenic belts containing mineral deposits. Together with the Junggar terrain they open an important window to study the Paleozoic tectonic evolution of the CAOB.
Zhiming Bai +5 more
doaj +1 more source
Characteristics of Carboniferous Volcanic Reservoirs in Beisantai Oilfield, Junggar Basin
In recent years, petroleum exploration in the Carboniferous volcanic rock reservoirs in the Junggar Basin has been the focus of important petroleum energy development in western China. The lithologic identification of volcanic rock reservoirs seriously restricts the accuracy of reservoir prediction and affects the success rate of oil exploration ...
Hanlie Cheng +5 more
openaire +1 more source

