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| 1 | 非弹性应变恢复法三维地应力测量——汶川地震科学钻孔中的应用显示文摘随着地球动力学和深部能源开发利用等研究工作的不断深入,深部应力状态的研究越来越重要,但目前尚没有即经济又简便完善的深部三维地应力测量方法.基于岩芯的非弹性应变恢复法是近年来发展起来的深部三维应力测量方法.汶川5·12地震后,中国大陆首次将该方法应用于科学钻孔的地应力测量.本文详细介绍了这一方法现场测量岩芯非弹性恢复应变的基本流程,并对此法测量的岩芯首次开展了岩石非弹性应变恢复柔量的实验研究,将现场非弹性应变测量与室内非弹性应变恢复柔量实验相结合,确定汶川地震科学钻一号孔(WFSD-1)1173 m处最大主应力方向为NW64°,实测得到岩石的剪切与体积模式非弹性应变恢复柔量的比值为2.9,计算得到最大、中间和最小主应力分别为43,28和25 MPa.结合龙门山地区其他方法的地应力测量结果,表明龙门山断裂带从NE到SW现今最大主应力作用方向表现为由EW→NEE→NWW的变化规律,龙门山断裂带现今地应力作用方向的分段性特征与5·12汶川地震时龙门山断裂带西南段逆冲为主,东北段走滑为主的运动特点相吻合,研究结果对于认识汶川地震的动力学机制具有一定参考价值. | 孙东生 WeiRen LIN 崔军文 王红才 陈群策 马寅生 王连捷 | 2014 | 中国科学:地球科学2014，44，3： | 12 |
| 2 | Porosity and permeability evolution and evaluation in anisotropic porosity multiscale-multiphase-multicomponent structure显示文摘Based on the hybrid hypersingular integral equation-lattice Boltzmann methods (HHIE-LBM), the porosity and permeability evolution and evaluation process in anisotropic saturated porosity multiscale-multiphase-multicomponent (ASP-MS-MP-MC) structures under ultra high temperature and pressure conditions was analyzed on parallel CPU and GPU platforms. First, virtual physical models at multi-spatial scales (2 μm, 5 μm and 10 μm) were restructured by computerized microtomography technology and data. Second, using HHIE-LBM methods, the anisotropic porosity and permeability tensor at core level and pore level under ultra high temperature and pressure conditions were calculated. Third, the evolution and evaluation process of the porosity and permeability as a function of multi temporal spatial scales was investigated. Finally, the relationship between porosity and permeability and ASP-MS-MP-MC structures (micro-meso-macro-scale) was explored. | ZHU BoJing CHENG HuiHong QIAO YanChao LIU Chang SHI YaoLin ZHANG Kai SUN DongSheng LIN WeiRen | 2012 | Chinese Science Bulletin2012，57，4： | 11 |
| 3 | Three-dimensional in situ stress determination by anelastic strain recovery and its application at the Wenchuan Earthquake Fault Scientific Drilling Hole-1(WFSD-1)显示文摘In situ stress state becomes more and more significant with in-depth research on geodynamics and energy development.However,there has not been an economic and effective method developed to determine deep three-dimensional in situ stress.The Anelastic Strain Recovery(ASR)method is a newly developed technique that can determine three-dimensional in situ stresses.After the 12 May 2008 Ms8.0 Wenchuan earthquake,the ASR method was used for the first time in China's Mainland to measure the in situ stresses in the WFSD scientific boreholes in Sichuan Province,China.In this paper,the basic procedure of the ASR method is introduced in detail and the compliances of ASR for boring cores are investigated.The results show that the maximum principal stress direction was NW64°at a measured depth(MD)of 1173 m(vertical depth 1151 m)in WFSD-1.The ratio of shear mode to the volume mode compliance of ASR was 2.9.And the three principal stresses at 1173 m MD in WFSD-1are 43,28 and 25 MPa.Combined with stress measurement results determined using other in situ measurement methods along the Longmenshan fault zone,the directions of the maximum horizontal principal stress changes from E-W to NEE-SWW to NWW-SEE when moving from NE to SW along the Longmenshan fault zone.This change is in agreement with the stress regime of the Longmenshan fault zone of the Wenchuan Earthquake,which supports a stress regime consisting predominantly of thrusts in the southwest and strike-slip in the northeast. | SUN DongSheng LIN WeiRen CUI JunWen WANG HongCai CHEN QunCe MA YinSheng WANG LianJie | 2014 | Science China Earth Sciences2014，57，6： | 10 |
| 4 | Bottom water temperature measurements in the South China Sea,eastern Indian Ocean and western Pacific Ocean显示文摘文章报道了一批新的海底底水温度(BWT)数据,其中南海(SCS)158个站位、东印度洋(EIO)30个站位及西太平洋(WPO)37个站位。基于这批新的BWT数据,获得南海和西太平洋海域底水温度与水深经验关系,可为地球物理和物理海洋提供准确、可靠的海底温度边界。这将有助于海底油气资源调查与评估。同时,这批实测数据表明:1)水深超过3500m的海域,其底水温度在南海约为2.47℃,比东印度洋(~1.34℃)和西太平洋(~1.60℃)稍微偏高。这与大洋传送带模式所预测的情况比较吻合。该模式认为:低温高盐的海水,从北大西洋格陵兰岛和冰岛附近海域下沉到深层,然后向南流动,再与南极洲周围海域的低温高盐海水一同向北进入印度洋和太平洋。而南海是一个相对比较封闭的热带边缘海,其内部海水与印度洋和菲律宾海交换有限,导致海水温度整体高于印度洋和太平洋。2)台西南盆地水深在2700~3000m的部分站位,其底水温高达约3.00℃,明显高于其周边同水深海域底水温度(平均值约为2.33℃)。这可能是台西南盆地海底水热活动导致的结果。3)在东印度洋和西太平洋水深超过4800m海域,底水温度随着水压增大稍有升高,其升高率分别为10.6mK·MPa^(-1)和12.0mK·MPa^(-1)。这与理论估算的深层底水绝热压力温度梯度范围较为吻合。这也意味着东印度洋和西太平洋深层底水,主要由绝热自压作用导致其温度随着深度的增大而升高。 | YANG Xiaoqiu SHI Xiaobin ZHAO Junfeng YU Chuanhai GAO Hongfang CHEN Aihua LU Yuanzheng CEN Xianrong LIN Weiren ZENG Xin XU Hehua REN Ziqiang ZHOU Shengqi XU Ziying SUN Jinlong KAMIYA Nana LIN Jian | 2018 | 热带海洋学报2018，37，5： | 8 |
| 5 | CFD simulation on the generation of turbidites in deepwater areas: a case study of turbidity current processes in Qiongdongnan Basin, northern South China Sea显示文摘Turbidity currents represent a major agent for sediment transport in lakes, seas and oceans. In particular, they formulate the most significant clastic accumulations in the deep sea, which become many of the world's most important hydrocarbon reservoirs. Several boreholes in the Qiongdongnan Basin, the northwestern South China Sea, have recently revealed turbidity current deposits as significant hydrocarbon reservoirs. However, there are some arguments for the potential provenances. To solve this problem, it is essential to delineate their sedimentary processes as well as to evaluate their qualities as reservoir. Numerical simulations have been developed rapidly over the last several years, offering insights into turbidity current behaviors, as geologically significant turbidity currents are difficult to directly investigate due to their large scale and often destructive nature. Combined with the interpretation of the turbidity system based on highresolution 3D seismic data, the paleotophography is acquired via a back-stripping seismic profile integrated with a borehole, i.e., Well A, in the western Qiongdongnan Basin; then a numerical model is built on the basis of this back-stripped profile. After defining the various turbidity current initial boundary conditions, including grain size, velocity and sediment concentration, the structures and behaviors of turbidity currents are investigated via numerical simulation software ANSYS FLUENT. Finally, the simulated turbidity deposits are compared with the interpreted sedimentary bodies based on 3D seismic data and the potential provenances of the revealed turbidites by Well A are discussed in details. The simulation results indicate that a sedimentary body develops far away from its source with an average grain size of 0.1 mm, i.e., sand-size sediment. Taking into account the location and orientation of the simulated seismic line, the consistence between normal forward simulation results and the revealed cores in Well A indicates that the turbidites should have been transported from Vietnam instead of Hainan Island. This interpretation has also been verified by the planar maps of sedimentary systems based on integration of boreholes and seismic data. The identification of the turbidity provenance will benefit the evaluation of extensively distributed submarine fans for hydrocarbon exploration in the deepwater areas. | JIANG Tao ZHANG Yingzhao TANG Sulin ZHANG Daojun ZUO Qianmei LIN Weiren WANG Yahui SUN Hui WANG Bo | 2014 | Acta Oceanologica Sinica2014，33，12： | 3 |
| 6 | Simultaneous generation of baseband and radio signals using only one single-electrode Mach-Zehn- der modulator with enhanced linearity显示文摘 | LIN Chunting PENG Weiren CHEN J | 2006 | IEEE Photonic Technology Let- ters2006，18，23： | 1 |
| 7 | Localized rotationof principal stress around faults and fractures determined fromborehole breakouts in hole B of the Taiwan Chelungpu-fault Drill-ing Project (TCDP) 显示文摘 | Lin Weiren Yeh Enchao Hung Jihhao | 2010 | Tectonophysics2010，482，14： | 1 |
| 8 | Localized rotation of principal stress around faults and fractures determined from borehole breakouts in hole B of the Taiwan Chelunpu-fault Drilling Project (TCDP) 显示文摘 | WEIREN LIN EN-CHAO YEH JIH-HAO HUNG | 2010 | Tectonophysics2010，482，14： | 1 |
| 9 | Molecular cloning and functional characterization of the first non-mammalian 26RFa/QRFP orthologue in Goldfish, Carassius auratus显示文摘 | Yun Liu Yong Zhang Shuisheng Li Weiren Huang Xiaochun Liu Danqi Lu Zining Meng Haoran Lin | 2009 | Molecular and Cellular Endocrinology2009，，1： | 1 |
| 10 | 日本南海海槽东部首次海上天然气试采站位滞弹性应变恢复法(ASR)在原位应力分析中的应用显示文摘原位应力可通过钻井岩心的滞弹性应变恢复(ASR)法来计算。在日本南海海槽东部首次海上天然气试采站位选取一口钻井,从海底之下265~313m之间不同深度取得四块岩心,在钻探船上进行滞弹性应变测量。现场ASR测量结果表明,该研究区深度范围内处于重力作用下形成的正断层应力状态。在随后的实验室实验中,通过K0固结法,使所取岩心恢复到原位应力状态,然后在卸压过程中和卸压之后进行弹性和滞弹性应力测量,进而验证现场(船上)测量结果和量化原位应力值。这些实验室校准实验验证了伴随着应力释放ASR测量结果可为人工预加压力提供合理的估计。 | Yu Nagano Weiren Lin Koji Yamamoto 任金锋 | 2017 | 海洋地质2017，0，1： | 0 |
| 11 | 2011年日本东北地区近海大地震最大位移区的应力状态显示文摘2011年MW9.0的日本东北地区近海大地震在日本海沟附近产生了最大超过50m的同震滑动,这可能导致该区域进入了应力近乎完全卸载的状态。为检验上述假设,我们利用综合大洋钻探计划在震后1年左右时间得到的钻孔资料,以及对震前应力状态的推断结果,确定了陆楔前缘的原地应力状态。根据孔壁崩落法对水平应力方向与应力大小的估算结果,以及在破裂向海沟轴方向传播过程中同震位移增大的现象,可推断原地水平应力在地震过程中变小了。这种应力变化显示出板块界面的前缘发生了相对自由的滑动,该结论与地震引起了断层弱化和发生了近乎全部的应力降等观测结果是吻合的。 | Weiren Lin Marianne Conin J Casey Moore Frederick M Chester Yasuyuki Nakamura James J Mori Louise Anderson Emily E Brodsky Nobuhisa Eguchi 343勘查队科技人员 冯万鹏(译) 许忠淮(校) | 2013 | 国际地震动态2013，，8： | 0 |
| 12 | Spatial and Temporal Stress Variations before and after the 2008 Wenchuan M_(w)7.9 Earthquake and its Implications:A Study based on Borehole Stress Data显示文摘In situ stress measurement data was analyzed to estimate the temporal and spatial stress variations at shallow depths in the Longmenshan fault zone(LMSF),prior to and following the 2008 Wenchuan earthquake(WCEQ).Analysis of the stress field related to fault strength and behavior is useful for understanding geodynamic processes and conducting hazard assessments.The shallow stress changes after the WCEQ show clear along-strike variations.Degrees of stress orientation rotations have a negative correlation with the horizontal principal stress ratios and the WCEQ apparently reduced the magnitude difference between horizontal principal stresses.Taking stress magnitudes and orientation distribution relative to the fault strike into account,we propose an intermediate-strength of LMSF,with a friction coefficient generally constrained between 0.35 and 0.6.In addition,high-pressure fluids in the fault zone reduce the effective normal stress and to a certain degree weaken the fault strength.The accumulated stress over a certain period following release of the WCEQ indicates the start of another earthquake cycle.The changing crustal stress field makes the LMSF stable or slipping optimally during geodynamic processes.The segmentation feature of the shallow crustal stress field in the LMSF may imply a different tectonic loading and seismic release processes along the fault.The southwestern section to the epicenter of the WCEQ favors the occurrence of future earthquakes,as highμm in a state of critical failure was present in this area,which indicates that the Wenchuan and Lushan earthquakes did not release the accumulated stress to a sufficient extent there. | MENG Wen LIN Weiren CHEN Qunce LI Yonghua | 2023 | Acta Geologica Sinica(English Edition)2023，97，1： | 0 |
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