Branding/Logomark minus Citation Combined Shape Icon/Bookmark-empty Icon/Copy Icon/Collection Icon/Close Copy 7 no author result Created with Sketch. Icon/Back Created with Sketch. Match!
  • References (59)
  • Citations (0)
Published on Jan 1, 2018in Gondwana Research 5.66
Yulia Vibe1
Estimated H-index: 1
(LMU: Ludwig Maximilian University of Munich),
Hans-Peter Bunge35
Estimated H-index: 35
(LMU: Ludwig Maximilian University of Munich),
Stuart R. Clark8
Estimated H-index: 8
(Simula Research Laboratory)
Abstract Vertical intraplate motions are not easily related to plate tectonics. Understanding their underlying mechanism is further complicated by poor constraints on the magnitude and timing of these motions. Western Siberia is a prominent intraplate area affected by vertical tectonics. Shortly after the assemblage of Pangaea, the region experienced substantial uplift followed by a long period of subsidence that led to formation of the world's largest sedimentary basin–the West Siberian Basin. ...
9 Citations Source Cite
Published on Oct 1, 2017in Journal of Asian Earth Sciences 2.87
Min He1
Estimated H-index: 1
(CNOOC Limited),
Guangfa Zhong9
Estimated H-index: 9
(Tongji University)
+ 4 AuthorsKe Huang1
Estimated H-index: 1
(Tongji University)
Abstract Data from 26 drill wells and 27 regional seismic profiles were integrated to investigate the timing, phase and origin of the post-rift subsidence in the middle to eastern Pearl River Mouth Basin (PRMB) of the northern South China Sea using the traditional 1-D backstripping technique. Different from previous research of backstripped tectonic subsidence in the basin, we calculated the tectonic subsidence using the newly built local porosity-depth relationships for decompaction and updated...
9 Citations Source Cite
Published on Dec 1, 2016in Tectonophysics 2.69
Jean-Claude Sibuet40
Estimated H-index: 40
(NTOU: National Taiwan Ocean University),
Yi-Ching Yeh12
Estimated H-index: 12
Chao-Shing Lee13
Estimated H-index: 13
(NTOU: National Taiwan Ocean University)
Abstract The beginning of seafloor spreading in the South China Sea (SCS) is now established from IODP drilling Leg 349 at 33 Ma. Chron 12 (32 Ma) is the oldest chron identified in the SCS. The nature of the crust of the northeastern part of the SCS located north of chron C12, where chrons 15 to 17 were previously identified, is not oceanic but thinned continental crust intruded by volcanic elongated features emplaced 17–22 Ma ago. Based on magnetic anomaly identifications, the end of the SCS sp...
50 Citations Source Cite
Published on Jan 1, 2016in Marine and Petroleum Geology 3.28
Gege Hui4
Estimated H-index: 4
(Ocean University of China),
Estimated H-index: 44
(Ocean University of China)
+ 6 AuthorsYibo Zang5
Estimated H-index: 5
(Ocean University of China)
Abstract The northern South China Sea (NSCS) experienced continuous evolution from an active continental margin in the late Mesozoic to a stable passive continental margin in the Cenozoic. It is generally believed that the basins in the NSCS evolved as a result of Paleocene–Oligocene crustal extension and associated rifting processes. This type of sedimentary environment provides a highly favourable prerequisite for formation of large-scale oil- and gas–fields as well as gas hydrate accumulation...
26 Citations Source Cite
Published on Nov 1, 2015in Marine and Petroleum Geology 3.28
Guangxue Zhang6
Estimated H-index: 6
Jinqiang Liang10
Estimated H-index: 10
+ 11 AuthorsHuaning Xu1
Estimated H-index: 1
Abstract Logging-while-drilling (LWD) and wireline log (CWL) data were acquired during China's second gas hydrate drilling expedition (GMGS-2) in the east of Pearl River Mouth Basin, South China Sea. Disseminated and massive gas hydrates deposits were found at different sites. Gas hydrate-bearing lithologies identified from the sample coring included the fine-grained sediments and coarse-grained sediments. LWD logs from Site GMGS2-08 indicate significant gas hydrate in clay-bearing sediments inc...
44 Citations Source Cite
Published on Sep 1, 2015in Journal of Asian Earth Sciences 2.87
Chao Li1
Estimated H-index: 1
(China University of Geosciences),
Shaofeng Liu18
Estimated H-index: 18
(China University of Geosciences)
To understand the formation mechanisms and evolution of the Songliao Basin, we applied backstripping and strain rate inversion methods to 20 wells and reinterpret two seismic sections in the Songliao Basin. The obtained data were used to reconstruct the tectonic subsidence history and further assess the potential subsidence mechanisms of this area. The predicted post-rift subsidence based on the uniform stretching model that followed earlier lithospheric thinning events was much lower than the s...
16 Citations Source Cite
Published on Jul 1, 2014in Journal of Asian Earth Sciences 2.87
Yanhui Suo18
Estimated H-index: 18
(Ocean University of China),
Estimated H-index: 44
(Ocean University of China)
+ 4 AuthorsLiming Dai18
Estimated H-index: 18
(Ocean University of China)
Abstract Tectonic migration is a common geological process of basin formation and evolution. However, little is known about tectonic migration in the western Pacific margins. This paper focuses on the representative Cenozoic basins of East China and its surrounding seas in the western Pacific domain to discuss the phenomenon of tectonic jumping in Cenozoic basins, based on structural data from the Bohai Bay Basin, the South Yellow Sea Basin, the East China Sea Shelf Basin, and the South China Se...
39 Citations Source Cite
Published on Mar 1, 2014in Tectonophysics 2.69
Hui Xie3
Estimated H-index: 3
(CAS: Chinese Academy of Sciences),
Di Zhou17
Estimated H-index: 17
(CAS: Chinese Academy of Sciences)
+ 5 AuthorsJinghe Cao19
Estimated H-index: 19
(CAS: Chinese Academy of Sciences)
The Cenozoic tectonic subsidence of the deepwater area in the Pearl River Mouth Basin, northern South China Sea is studied by subsidence analysis via backstripping calculations based on data of newly interpreted sequence boundaries. In the subsidence analysis local porosity-depth parameters were estimated based on well data, the paleo-water depth parameters and lithology were estimated for all grid nodes based on well data and sedimentary system maps, and ages of sequence boundaries were adjuste...
57 Citations Source Cite
Published on Apr 3, 2013
Brian Taylor11
Estimated H-index: 11
(Columbia University),
Dennis E. Hayes38
Estimated H-index: 38
(Columbia University)
638 Citations Source Cite
Published on Mar 19, 2013
Martin F. J. Flower27
Estimated H-index: 27
(UIC: University of Illinois at Chicago),
Kensaku Tamaki27
Estimated H-index: 27
(UTokyo: University of Tokyo),
Hoang Nguyen8
Estimated H-index: 8
(UTokyo: University of Tokyo)
131 Citations Source Cite
Cited By0