Nansheng Qiu

ORCID: 0000-0001-8092-0410
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About
Contact & Profiles
Research Areas
  • Hydrocarbon exploration and reservoir analysis
  • Geological and Geochemical Analysis
  • Geological and Geophysical Studies
  • Geological Studies and Exploration
  • Geochemistry and Geologic Mapping
  • High-pressure geophysics and materials
  • Methane Hydrates and Related Phenomena
  • earthquake and tectonic studies
  • Hydraulic Fracturing and Reservoir Analysis
  • Petroleum Processing and Analysis
  • Atmospheric and Environmental Gas Dynamics
  • Geothermal Energy Systems and Applications
  • NMR spectroscopy and applications
  • Seismic Imaging and Inversion Techniques
  • Geological formations and processes
  • Geology and Paleoclimatology Research
  • Paleontology and Stratigraphy of Fossils
  • Coal Properties and Utilization
  • Enhanced Oil Recovery Techniques
  • Geochemistry and Geochronology of Asian Mineral Deposits
  • Geochemistry and Elemental Analysis
  • Reservoir Engineering and Simulation Methods
  • Geological Modeling and Analysis
  • Cyclone Separators and Fluid Dynamics
  • Coal and Its By-products

China University of Petroleum, Beijing
2016-2025

Jiangsu University
2024

Sinopec (China)
2006-2015

China National Petroleum Corporation (China)
2008

Research Institute of Petroleum Exploration and Development
2008

Ministry of Education of the People's Republic of China
2005-2006

Sheng Jing Hospital
2002

Institute of Geology and Geophysics
1993

The Tarim Basin is one of the richest basins in oil and gas resources China. Cambrian Middle–Upper Ordovician strata are most important source rocks. Previous early Paleozoic thermal histories have led to varied hypotheses on evolution lower rocks, causing a significant impact petroleum exploration basin. A new history was reconstructed this article using integrated indicators apatite zircon (uranium-thorium)/helium ages, fission tracks, equivalent vitrinite reflectance data. modeled results...

10.1306/09071111029 article EN AAPG Bulletin 2012-04-30

The offshore Bohai Bay Basin, located in the central north China, one of most petroliferous basins China. In this article, based on formation-testing temperature, drill-stem tests, and bottom-hole temperature data, 80 thermal gradient values at depth interval 0 to approximately 3000 m (~9843 ft) Basin were obtained. basinwide average is 31.8 4.6C/km. Based above data corresponding weighted conductivity measured terrestrial heat flow These range from 33.5 84.0 mW/m2, with an value 60.8 8.7...

10.1306/09271010079 article EN AAPG Bulletin 2011-05-01

The Sichuan Basin is a prime gas-producing basin in China. Besides the giant Neoproterozoic Weiyuan gas field discovered central paleo-uplift, an extra reservoir Cambrian this area has been confirmed recent years. Although lower Paleozoic southwest (Weiyuan area) normally pressured, it overpressured (Moxi–Gaoshiti area). Combined with seal distribution, five pressure systems, including three overpressure can be divided based on drill-stem test, mud weight, and sonic transit time data....

10.1306/02101614037 article EN AAPG Bulletin 2016-05-01

The Tarim Basin is one of the most important hydrocabon-bearing evaporite basins in China. Four salt-bearing sequences, Middle and Lower Cambrian, Mississippian, Paleogene, Neogene, have various thickness areal distribution. They are detachment layers intensely affect structural deformation basin. Kuqa depression a subordinate unit with abundant salt structures Basin. Salt overthrusts, pillows, anticlines, diapirs, salt-withdrawal predominant depression. Contraction that resulted from...

10.1306/05301311156 article EN AAPG Bulletin 2013-12-20

This article discusses the Meso–Cenozoic thermal history, lithospheric thinning, and structure of lithosphere Bohai Bay Basin, North China. The present-day regime basin features an average heat flow 64.5 ± 8.1 mW m–2, a thickness 76–102 km, ‘hot mantle but cold crust’-type structure. history experienced two peaks in late Early Cretaceous middle to Palaeogene, with values 82–86 m‒2 81–88 m‒2, respectively. Corresponding these peaks, thinning stages during reaching minimum 43–61 km....

10.1080/00206814.2014.1002818 article EN International Geology Review 2015-02-04

Abstract Cenozoic exhumation in the Tianshan is controlled by a complex interaction between tectonics and climate. However, timing magnitude of its contribution to climate change Central Asia remains debated. In this study, we report new apatite fission track (U‐Th)/He ages for granite samples from roof South that are significantly younger than those published other parts Tianshan. Inverse forward modeling reveals two phases accelerated cooling at 10∼6 Ma since ∼3 Ma, which can be linked (1)...

10.1029/2020gl090623 article EN Geophysical Research Letters 2020-12-29
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