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Zhao Hongge
Northwest University (United States)
15Publications
6H-index
129Citations
Publications 14
Newest
#1Chiyang Liu (Northwest University (United States))H-Index: 6
#2Lei Huang (Northwest University (United States))H-Index: 3
Last.Changyu Fan (Northwest University (United States))H-Index: 2
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A large number of small-scale lacustrine sedimentary basins are widely distributed across China. Studies of such basins have been limited. These basins have complex characteristics and thus exhibit significant differences in terms of their hydrocarbon potential. At present, among the known 348 small-scale basins with areas less than 20,000 km2 ( 200 m/m.y. [>656 ft/m.y.]) during deposition of the source rocks within underfilled and balanced-filled lakes.
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#2Liu ChiyangH-Index: 8
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#1Zhao Hongge (Northwest University (United States))H-Index: 6
#2Chiyang Liu (Northwest University (United States))H-Index: 4
Last.Hairan Wang (Northwest University (United States))H-Index: 1
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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...
9 CitationsSource
#1Liu Chiyang (Northwest University (United States))H-Index: 8
#2Zhao Hongge (Northwest University (United States))H-Index: 6
Last.Yang Minghui (China University of Petroleum)H-Index: 5
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: The Ordos basin was developed from Mid-Late Triassic to Early Cretaceous, and then entered into its later reformation period since the Late Cretaceous. Its main body bears the features of an intra-cratonic basin. The basin also belongs to a multi-superposed basin which has overlapped on the large-scale basins of the Early and Late Paleozoic. Currently, Ordos basin has become a residual basin experienced reformation of various styles since the Late Cretaceous. It's suggested that there were at ...
27 CitationsSource
Based on the study of stratigraphic characteristics,sedimentary features and tectonic deformation, combined with the analysis of apatite fission rack dating,etc,it was suggested that the Weibei uplift had experienced a significant late reformation,which constituted the main part of the Ordos basin,and generally accepted deposition before the end of early cretaceous without the development of uplift.As a positive tectonic unit it should have started between the end of early cretaceous and late cr...
3 Citations
#1Chiyang LiuH-Index: 1
#2Xinwei QiuH-Index: 1
Last.Zhao Hongge (Northwest University (United States))H-Index: 6
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More than 82 percent of confirmed sandstone-type uranium deposits coexist with confirmed oil-gas or coalfields in the world, which reflects a ubiquitous phenomenon of coexistence and accumulation of multi-energy minerals including oil, gas, coal and uranium in the same basin. It happens mostly in the Central-east Asia energy basins. Across China, Mongolia and some central Asian countries, the giant Central-east Asia metallogenetic domain (CEAMD) stretches for more than 6000 km, from Songliao Bas...
8 CitationsSource
#1Zhao Hongge (Northwest University (United States))H-Index: 6
#2Chiyang Liu (Northwest University (United States))H-Index: 4
Last.Meiyan Liang (CAS: Chinese Academy of Sciences)H-Index: 1
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Ordos Block is considered as a rather stable basin in Cenozoic by most researchers. The result of our study is different from this opinion. Before the Cenozoic, tectonic movement directions are uplifted in the eastern part and sunk in the western part of the basin. The oldest Cenozoic strata which deposit in the east part of Ordos Basin are Neogene red clays. They appear on both Pre-Tertiary and Post-Mesozoic geological maps of Ordos Basin. According to fission track dating data from various res...
4 CitationsSource
#1Chiyang Liu (Northwest University (United States))H-Index: 4
#2Zhao Hongge (Northwest University (United States))H-Index: 6
Last.Yuzhuang Sun (Hebei University of Engineering)H-Index: 9
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In order to study the relationship of energy mineral deposits and tectonic movements in Ordos basin, more than 82 samples were taken for determination of apatite and zircon fission tracks. Furthermore, 93 apatite and zircon fission tracks have been selected from other publications. According to these data and other geological background, the evolution of Ordos basin can be divided into 4 stages, and the reformation of the basin can be divided into 5 stages. The basin formation and development we...
35 CitationsSource
#1Zhao Hongge (Northwest University (United States))H-Index: 6
According to the different characteristics of regional structures, basin's evolutions and mineralization conditions, the Central-East Asia energy minerals metallogenetic domain (CEAMD) can be divided into such four mineralization zones as Songliao-Ordos, Alashan-Hexi corridor, Xinjiang and Central Asia ones. The comprehensive analyses and comparisons of accumulation/mineralization conditions and current exploration of multi-energy minerals show that the relatively stable regional tectonic backgr...
#1Liu ChiyangH-Index: 8
#2Zhao HonggeH-Index: 6
Last.Wang JianqiangH-Index: 4
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