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Geometry and 3D seismic characterisation of post-rift normal faults in the Pearl River Mouth Basin,northern South China Sea
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作者 Yuanhang Liu Jinwei Gao +2 位作者 Wanli Chen Jiliang Wang Umair Khan 《Acta Oceanologica Sinica》 SCIE CAS CSCD 2024年第4期25-39,共15页
Based on high-resolution 3D seismic data acquired in the Pearl(Zhujiang)River Mouth Basin of the northern South China Sea,this study investigated the geometry,spatial extension,and throw distribution of the post-rift ... Based on high-resolution 3D seismic data acquired in the Pearl(Zhujiang)River Mouth Basin of the northern South China Sea,this study investigated the geometry,spatial extension,and throw distribution of the post-rift normal fault through detailed seismic interpretation and fault modeling.A total of 289 post-rift normal faults were identified in the study area and can be classified into four types:(1)isolated normal faults above the carbonate platform;(2)isolated normal faults cutting through the carbonate platform;(3)conjugate normal faults,and(4)connecting normal faults.Throw distribution analysis on the fault planes show that the vertical throw profiles of most normal fault exhibit flat-topped profiles.Isolated normal faults above the carbonate platform exhibit roughly concentric ellipses with maximum throw zones in the central section whereas the normal faults cutting through the carbonate platform miss the lowermost section due to the chaotic seismic reflections in the interior of the carbonate platform.The vertical throws of conjugate normal faults anomalously decrease toward their intersection region on the fault plane whereas the connecting normal faults present two maximum throw zones in the central section of the fault plane.According to the symmetric elliptical distribution model of fault throw,an estimation was made indicating that normal faults cutting through the carbonate platform extended downward between-1308 s and-1780 s(two-way travel time)in depth and may not penetrate the entire Liuhua carbonate platform.Moreover,it is observed that the distribution of karst caves on the top of the carbonate platform disaccord with those of hydrocarbon reservoirs and the post-rift normal faults cutting through the carbonate platform in the study area.We propose that these karst caves formed most probably by corrosive fluids derived from magmatic activities during the Dongsha event,rather than pore waters or hydrocarbons. 展开更多
关键词 Post-rift normal faults fault throw Karst caves Corrosive fluids Pearl River Mouth Basin South China Sea
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CORROSION FATIGUE CRACK INITIATION BEHAVIOR OF 316L STAINLESS STEEL IN HANK’S SOLUTION
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作者 J.H. Xie Y.S. Wu +1 位作者 J.Q. He X.Z.Yang and R.Z. Zhu (Department of Surface Science & Corrosion Engineering, University of Science and Technology Beijing,Beijing 100083, China) 《Acta Metallurgica Sinica(English Letters)》 SCIE EI CAS CSCD 1996年第5期333-337,共5页
This paper investigates the corrosion fatigue (CF) crack initiation behavior of 316L stainless steel in Hank's solution which simulates bodylike fluid. The CF experiments were conducted under the conditions of ele... This paper investigates the corrosion fatigue (CF) crack initiation behavior of 316L stainless steel in Hank's solution which simulates bodylike fluid. The CF experiments were conducted under the conditions of electrochemically accelerated, free immersion and pre-polarized pitting potential. The results showed that 316L stainless steel was susceptible to pitting corrosion in Hank's solution. Intergranular corrosion occurred obviously at the bottom of pits where the CF cracks initiated by the combined action of alternating stress and corrosive medium for the notch effect of stress concentrated in the grain boundaries.The CF crack propagation is both intergranular and transgranular. 展开更多
关键词 aritificial joints 316L stainless steel simulated bodylike fluid corrosion fatigue pitting corrosion intergranular corrosion
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高演化海相碳酸盐岩层系古温标的直接指标——包裹体均一温度 被引量:10
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作者 秦建中 饶丹 蒋宏 《石油实验地质》 CAS CSCD 北大核心 2008年第5期494-498,共5页
对川东北地区多口钻井岩心样品包裹体均一温度、盐度、密度等的系统分析发现,该地区具有3期烃类流体活动的迹象。包裹体均一温度与盐度、密度具有较好的相关性,在古今地温梯度变化不大的情况下,可以利用实测包裹体均一温度与古地温梯度... 对川东北地区多口钻井岩心样品包裹体均一温度、盐度、密度等的系统分析发现,该地区具有3期烃类流体活动的迹象。包裹体均一温度与盐度、密度具有较好的相关性,在古今地温梯度变化不大的情况下,可以利用实测包裹体均一温度与古地温梯度推算当时的最大埋深或剥蚀厚度,恢复其热演化历史。储层最高包裹体均一温度与镜质体反射率、实测地温、伊利石结晶度等多项指标均具有较好的相关性,是现今开展海相高演化地区热史恢复的一项直接、有效的指标。 展开更多
关键词 包裹体均一温度 热演化指标 剥蚀厚度 热史恢复 川东北地区
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