Results 31 to 40 of about 548 (192)

Coupled onshore erosion and offshore sediment loading as causes of lower crust flow on the margins of South China Sea [PDF]

, 2015
© 2015, Clift. Hot, thick continental crust is susceptible to ductile flow within the middle and lower crust where quartz controls mechanical behavior.
Peter D. Clift
core   +4 more sources

A new kinetic model for authigenic quartz formation under overpressure

Petroleum Exploration and Development, 2013
To model the change of authigenic quartz content precisely in geological history, a new kinetic model combining time, temperature and pressure was established considering the retardation of overpressure to the formation of authigenic quartz on the basis ...
Yuanlin MENG, Cheng XU, Hongyu XIE, Weizhi TIAN, Chuanxin TONG, Jinghuan LIU, Youchun WANG, Yuting GAO   +7 more
doaj   +1 more source

Seismic sedimentology of submarine fan system in the 1st Member of the Huangliu Formation, Dongfang area, Yinggehai Basin, China

地质科技通报, 2023
Objective The Yinggehai Basin's Dongfang area is a significant area for oil and gas exploration, characterized by the presence of large-scale submarine fan complexes.
Yayun Dang
doaj   +1 more source

CO2 Fluid Flow Patterns near Major Deep Faults: Geochemical and 3D Seismic Data from the Ying‐Qiong Basin of the South China Sea

Geofluids, Volume 2022, Issue 1, 2022., 2022
CO2 and hydrocarbon fluids typically migrate from deeper layers into the shallow crust via large deep faults. Consequently, CO2, hydrocarbon, and water reservoirs tend to occur in traps near deep and large faults. In this study, we use structural and stratigraphic data to identify and predict CO2 and hydrocarbon gas reservoirs near major deep faults ...
Junfeng Yu, Ruiyou Song, Jianxiang Pei, Qilin Wu, Yuan Shao, Wei Zhang   +5 more
wiley   +1 more source

Wrench-Slip Reversals and Structural Inversions: Cenozoic Slide-Rule Tectonics in Sundaland [PDF]

, 2014
DOI: 10.17014/ijog.v1i1.174Most of continental Southeast Asia, that is, Sundaland and Indosinia, achieved a relative tectonic stability by the beginning of the Cenozoic.
Tjia, H. D. (H)
core   +1 more source

A tuffaceous volcaniclastic turbidite bed of Early Miocene age in the Temburong Formation of Labuan, North‐West Borneo and its implications for the Proto‐South China Sea subduction in the Burdigalian

The Depositional Record, Volume 7, Issue 1, Page 111-146, February 2021., 2021
A smectite bed in a sequence of distal, deep water turbidites and marine mudstones of the Temburong Formation on the island of Labuan, Sabah, North‐West Borneo is interpreted as an altered, re‐sedimented pyroclastic tuff which is geochemically of dacite‐rhyolite composition.
Stuart D. Burley, H. Tim Breitfeld, David ‘Stan’ Stanbrook, Robert J. Morley, Jochen Kassan, Mohamad Sukarno, D. Wantoro Wantoro   +6 more
wiley   +1 more source

Geological Characteristics of Mud Volcanoes and Diapirs in the Northern Continental Margin of the South China Sea: Implications for the Mechanisms Controlling the Genesis of Fluid Leakage Structures

Geofluids, Volume 2021, Issue 1, 2021., 2021
Mud volcanoes and diapirs are geological structures formed due to arch piercing or diapiric intrusion of ductile sedimentary materials into the overlying strata along high permeability channels. A detailed study on the processes controlling the formation of mud volcanoes and diapirs in the northern continental margin of the South China Sea is of vital ...
Siling Zhong, Jinfeng Zhang, Junsheng Luo, Yajuan Yuan, Pibo Su, Priyank Jaiswal   +5 more
wiley   +1 more source

Source-to-Sink Comparative Study between Gas Reservoirs of the Ledong Submarine Channel and the Dongfang Submarine Fan in the Yinggehai Basin, South China Sea

Energies, 2022
The Ledong submarine channel and the Dongfang submarine fan, two remarkable sedimentary systems developed during the late Miocene, are considered promising hydrocarbon reservoirs in the Yinggehai Basin of the South China Sea.
Yue Yao, Qiulei Guo, Hua Wang
doaj   +1 more source

The effect of thermal fluid derived from mud diapir on sandstone reservoirs in the Yinggehai Basin, South China Sea

Energy Geoscience, 2022
The underground thermal fluid is one of the significant factors controlling the formation and quality of reservoirs. The Huangliu Formation (N1h) in YF1 area of the central depression belt in the Yinggehai Basin, South China Sea, is characterized by ...
Xiaowei Lv, Meiyan Fu, Shaonan Zhang, Yi Liu, Xiaoqi Ding, Xianghao Meng, Shuai Yin, Tengjiao Sun   +7 more
doaj   +1 more source

Controlling Factors of Overpressure Formation in the Yinggehai Basin

Energy Exploration & Exploitation, 2012
There are many previous studies on the formation mechanism of overpressure in sedimentary basins. The Yinggehai Basin is a typical strike-slip extensional basin with obvious overpressure phenomenon. Yinggehai Formation begins to appear overpressure in Central Diapir Zone with the depth of less than 2000 m.
Wan Zhifeng, Xia Bin, Shi Qiuhua, Guo Feng, Cai Song   +4 more
openaire   +1 more source