Results 161 to 170 of about 628,563 (215)

The Characteristics of Heat Flow and Geothermal Field in Junggar Basin

Chinese Journal of Geophysics, 2000
AbstractBased on the temperature data of 196 wells and measurements of 90 thermal conductivity of rocks in Junggar basin, 35 terrestrial heat flow values are presented. The results show that the Junggar basin is a relatively "cold basin" at present, in which both temperature gradient and heat flow are lower.
Ji-Yang Wang
exaly   +2 more sources

Origin and charging histories of diagenetic traps in the Junggar Basin

AAPG Bulletin, 2021
ABSTRACT Oil and gas accumulations in the sandy conglomerate diagenetic traps that developed in the fan delta of the Triassic Baikouquan Formation of the Mahu sag, Junggar Basin, differ from stratigraphic accumulations controlled by sedimentary facies.
Jianguo Pan   +9 more
openaire   +1 more source

End Late Paleozoic tectonic stress field in the southern edge of Junggar Basin [PDF]

open access: yesGeoscience Frontiers, 2012
This paper presents the end Late Paleozoic tectonic stress field in the southern edge of Junggar Basin by interpreting stress-response structures (dykes, folds, faults with slickenside and conjugate joints).
Wei JU, Guiting Hou
exaly   +2 more sources

Petroleum in the Junggar basin, northwestern China

Journal of Southeast Asian Earth Sciences, 1988
Abstract The Junggar basin occupies a large triangular area of some 130 000 km2 in northwestern China. Situated between the Altay Shan (Altay Range) on the northeast and the Tian Shan (Tian Range) on the southwest, and between lesser ranges around the remainder of its periphery, the Junggar basin is completely intermontane.
Irfan Taner   +2 more
openaire   +1 more source

Basement structure and properties of the southern Junggar Basin

Journal of Geodynamics, 2018
Abstract We have investigated the detailed structures of velocity, density and magnetization intensity along a nearly east-west profile from Liugou to Dajing across the southern Junggar Basin using the seismic converted wave profiling and joint inversion of gravity and geomagnetic data. Our observations reveal such important interfaces as interface B
Junmeng Zhao   +6 more
openaire   +1 more source

Tectonic Evolution and Petroleum Systems in the Junggar Basin

Acta Geologica Sinica - English Edition, 2004
Abstract  The Junggar basin is located in the northern part of Xinjiang of China. It is part of the Kazakstan plate, surrounded by the Paleozoic folded mountains: the Halaart, Zayier and Chepaizi Mountains in the northwest, the Qingelidi and Karamaili Mountains in the northeast, and the Tianshan Mountains in the south.
WANG Weifeng, CHEN Yequan
openaire   +1 more source

Integrated Fracture Delineation in Volcanics, Junggar Basin, China

Advanced Materials Research, 2014
Fracture effectiveness, extension and connectivity from borehole surface into deep formation are the key factors to control producibility of volcanic formations. A systematic and integrated fracture delineation approach was set up which integrated available measurements with multi-scale depth of investigation to cover borehole surface, near wellbore ...
Fang Fang Wu   +3 more
openaire   +1 more source

Thermal history of the periphery of the Junggar Basin, Northwestern China

Organic Geochemistry, 1994
Abstract Geochemical analysis of rock core samples show that the basin periphery has experienced low thermal stress; present-day heat flows are in the range of 25–35 mW/m2 and have not been significantly higher than the worldwide mean of approx. 63 mW/m2 since the mid-Permian.
J.David King, Jianqiang Yang, Fan Pu
openaire   +1 more source

Characteristics and Origin of Conglomerate Diagenetic Traps in the Junggar Basin

Proceedings, 2018
Summary Oil-gas reservoirs in sandy conglomerate diagenetic traps, developed in the fan delta of the Triassic Baikouquan Formation, Mahu sag, Junggar Basin, are different from lithologic reservoirs controlled by sedimentary facies. In this study, mineralogical and petrological data are employed to evaluate formation.
W. Guodong   +3 more
openaire   +1 more source

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