Match!
Jianqiang Wang
Northwest University (United States)
11Publications
3H-index
78Citations
Publications 11
Newest
#1Heng Peng (Northwest University (United States))H-Index: 1
#2Jianqiang Wang (Northwest University (United States))H-Index: 3
Last.Qi Feng (Northwest University (United States))
view all 7 authors...
Abstract The Cenozoic outward growth of the Tibetan Plateau is traditionally considered to be responsible for the arcuate structures in the northeastern Tibetan Plateau. However, it is still unclear how pre-Cenozoic tectonics contributed to this unique geomorphic setting. To decipher the Meso-Cenozoic tectonic evolution, we systematically summarize the published thermochronological data and perform a low-temperature thermochronology study on Paleozoic-Mesozoic samples from the Haiyuan-Liupanshan...
#1Ming Ma (Northwest University (United States))
#2Chiyang Liu (Northwest University (United States))H-Index: 5
Last.Quanyun Miao (China University of Petroleum)
view all 7 authors...
#1Chiyang Liu (Northwest University (United States))H-Index: 5
#2Lei Huang (Northwest University (United States))H-Index: 3
Last.Jianqiang Wang (Northwest University (United States))H-Index: 3
view all 8 authors...
The Bohai Bay and Hehuai (southern North China) rift basins in the eastern part of the North China Craton are south-north-adjacent. They have shown synchronous evolutionary processes, and possess generally identical superficial and shallow structural characteristics as well as similar basin areas. However, there is a large difference in the richness of oil resources between the two basins. The Bohai Bay Basin has extremely abundant oil reserves, while commercial oil reserves have not been found ...
#1Pei Guo (Northwest University (United States))
#2Chiyang Liu (Northwest University (United States))H-Index: 5
Last.Yu Deng (Northwest University (United States))H-Index: 3
view all 4 authors...
U–Pb detrital zircon data from the Jurassic strata in the western Ordos Basin (WOB) show significant age differences between formations, from lower to upper including the Yan'an, Zhiluo, Anding, and Fenfanghe formations. The main peaks in the detrital zircon age spectra of the Yan'an Formation are at ca. 245, 444, 1813, and 2,387 Ma, which resemble those of the underlying Triassic strata in the WOB. Combined with the occurrence of reworked sporopollen and carbonate debris, the sediments of the Y...
#1Pei Guo (Northwest University (United States))
#2Chiyang Liu (Northwest University (United States))H-Index: 4
Last.Wenqing Wang (Northwest University (United States))
view all 6 authors...
Abstract The western Ordos Basin (WOB), situated in a tectonic transition zone in the North China Craton, acts as an excellent example for studying the Mesozoic intraplate sedimentation and deformation in Asia. In this study, U-Pb ages for 1203 detrital zircons of 14 sandstone samples collected from 11 sections are presented to unravel the sediment source locations and paleogeographic environments of the Early–Middle Jurassic coal-bearing Yan'an Formation in the WOB. Data show that there are fiv...
#1Xinwei Qiu (Northwest University (United States))H-Index: 1
#2Chiyang Liu (Northwest University (United States))H-Index: 4
Last.Jianqiang Wang (Northwest University (United States))H-Index: 3
view all 6 authors...
Abstract The Upper Triassic Chang 7 non-marine hot shales have been proven to contribute to Mesozoic oil reservoirs in the Ordos basin, Central China. These shales have been studied extensively in sedimentology, petrology and organic geochemistry. However, the factors controlling the development of the shales are still ambiguously constrained. This paper presents the major, trace, and platinum-group elements (PGEs) data to address these issues. The Chemical Index of Alteration (CIA), Chemical In...
#1Xinwei Qiu (CAS: Chinese Academy of Sciences)H-Index: 3
#2Chiyang Liu (Northwest University (United States))H-Index: 4
Last.Jianqiang Wang (Northwest University (United States))H-Index: 3
view all 6 authors...
Abstract Tuff intervals of Upper Triassic Yanchang Formation are laterally widespread in the Ordos basin, Central China. This paper focuses on magmatic origins and potential source regions of these tuff intervals through detail depositional, petrographic and geochemical analyses. Most of the tuff intervals are well-documented at the bottom of the Chang7 oil reservoir unit and can be correlated laterally, and certain tuff beds are reworked by turbidity current or seismic activity. Petrographic st...
#1Zhao Hongge (Northwest University (United States))H-Index: 6
#2Chiyang Liu (Northwest University (United States))H-Index: 3
Last.Hairan Wang (Northwest University (United States))H-Index: 1
view all 6 authors...
Ordos Basin, rich in multi-energy resources of oil, gas and uranium, is a depression basin within the Late Triassic-to-early Cretaceous craton, which overlapps on the Paleozoic craton basin. The basin started its later reformation in the Late Cretaceous, which is of significant importance to energy deposits. Few studies have, however, been focused on ages of the reformation and its characteristics. Based on the analysis of the regional geological settings and Cenozoic sedimentary structures, com...
12