ASR和DITF法综合确定塔里木盆地7 km深部地应力状态

doi:10.13722/j.cnki.jrme.2016.1145

摘要
图/表
参考文献
相关文章 (15)

全文: PDF (2100 KB) HTML (1 KB)
输出: BibTeX | EndNote (RIS)

摘要针对塔里木盆地致密气勘探开发中地应力测试需求，利用非弹性应变恢复(ASR)和钻井诱发裂缝(DITF)地应力测试方法，分析塔里木盆地7 km深部的地应力状态。研究表明：(1) SN-X井6 293～6 955 m深度范围内最大主应力近垂直，中间和最小主应力近水平，最大水平主应力方向在N E 51°～79°范围。(2) 在区域挤压构造环境下，塔里木盆地内部存在与碰撞造山后应力松弛或构造旋转逃逸引起的正断层应力环境。(3) 通过与DITF法地应力测量结果的对比分析，验证了ASR法用于7 km深部地应力测量的有效性，预期ASR法以其成本低、效率高且不受钻井深度和温度限制的优点，在深部科学钻探、非常规油气开发及地热资源开发等领域具有广阔的应用前景。

	服务

	把本文推荐给朋友
	加入我的书架
	加入引用管理器
	E-mail Alert
	RSS
	作者相关文章
	孙东生1
	吕海涛2
	王连捷1
	崔军文3
	何碧竹3
	曹自成2
	邱华标2
	颜修刚2

关键词 ：岩石力学, 地应力, 非弹性应变恢复法, 钻井诱发张裂缝, 正断层应力环境

Abstract：To obtain the state of in-situ stress during the exploration of dense gas reservoir under Tarim Basin，the anelastic strain recovery(ASR) and the methods of drilling induced tensile fractures(DITF) were applied to measure the in-situ stress at depth of 7 km. The results show that the maximum principle stress is close to vertical and the medium and the minimum principle stresses are close to horizontal in SN-X well at 6 293–6 955 m depth. The orientation of maximum horizontal principal stress is NE51°–NE79°. The normal faulting stress regime exists in the inner Tarim Basin caused possibly by the stress releasing after the orogenic period or the escaping structures of Tarim basin by the long distance effect of Himalaya collisional orogeny. The effectiveness of ASR method at the ultra-depth was confirmed by the close results from the ASR and DITF methods. The ASR method has the advantages of low cost，high efficiency，and no depth and temperature limitation，and hence，will have broad prospect of application at ultra-depth in scientific drilling，unconventional oil and gas exploration and geothermal development.

Key words： rock mechanics in-situ stress anelastic strain recovery method drilling induced tensile fractures normal faulting stress regime

引用本文:

孙东生1，吕海涛2，王连捷1，崔军文3，何碧竹3，曹自成2，邱华标2，颜修刚2. ASR和DITF法综合确定塔里木盆地7 km深部地应力状态[J]. 岩石力学与工程学报, 2018, 37(2): 383-391.
SUN Dongsheng1，LYU Haitao2，WANG Lianjie1，CUI Junwen3，HE Bizhu3，CAO Zicheng2，QIU Huabiao2，YAN Xiugang2. Determination of the in-situ stress state at 7 km depth under Tarim Basin by ASR and DITH methods. , 2018, 37(2): 383-391.

链接本文:

http://www.rockmech.org/CN/10.13722/j.cnki.jrme.2016.1145 或 http://www.rockmech.org/CN/Y2018/V37/I2/383

[22]	Vishay Precision Group. Measurement of thermal expansion coefficient using strain gages[J]. Micro-Measurement，2010，Tech Note TN-513-1：119-129.
[18]	袁俊文. 顺南501井钻井液技术[J]. 化工管理，2015，28(5)：116-117.(YUAN Junwen. The drilling mud technique of SN501 wellbore[J]. Chemical Enterprise Management，2015，28(5)：116-117.(in Chinese))
[28]	LADERIAN A. Prediction of temperature profile in oil wells[J]. International Journal of Engineering，2000，13：77-89.
[34]	CARROL LA R，GRAHAM S A，SMITH M E. Walled sedimentary Basins of China[J]. Basin Research，2010，22：17-32.
[4]	ZENG L B，WANG H J，LEI G，et al. Impacts of the tectonic stress field on natural gas migration and accumulation：a case study of the Kuqa Depression in the Tarim Basin，China[J]. Marine and Petroleum Geology，2010，27：1 616-1 627.
[14]	SUN D S，LIN W R，CUI J W，et al. Three-dimensional in situ stress determination by anelastic strain recovery and its application at the Wenchuan earthquake fault scientific drilling hole-1(WFSD-1)[J]. Science China：Earth Sciences，2014，57(6)：1 212-1 220.
[24]	MATSUKI K. Anelastic strain recovery compliance of rocks andits application to in situ stress measurement[J]. International Journal of Rock Mechanics and Mining Science，2008，45(6)：952-965.
[2]	FINKBEINER T，BARTON C A，ZOBACK M D. Relationships among in-situ stress，fractures and faults，and fluid flow：monterey formation，santa maria basin，california[J]. AAPG Bulletin，1997，81：1 975-1 999.
[6]	BRUDY M，ZOBACK M D，FUCHS K，et al. Estimation of the complete stress tensor to 8 km depth in the KTB scientific drill holes：Implications for crustal strength[J]. Journal of Geophysical Research，1997，102(B8)：18 453-18 475.
[8]	孙东生，丰成君，许洪斌，等. 大台沟矿区深孔水压致裂原地应力测量与应用[J]. 中南大学学报：自然科学版，2015，46(4)：1 384- 1 392.(SUN Dongsheng，FENG Chengjun，XU Hongbin，et al. In-situ stress measurement at deep borehole of Dataigou iron mine area and its application[J]. Journal of Central South University：Science and Technology，2015，46(4)：1 384-1 392.(in Chinese))
[9]	MATSUKI K. Three-dimensional in-situ stress measurement with anelastic strain recovery of a rock core[C]// Proceedings of the 7th International Congress on Rock Mechanics. Aachen，Deutschland：CRC Press，1991：557-560.
[12]	林为人. 基于岩芯非弹性应变恢复量测定的深孔三维地应力测试方法[J]. 岩石力学与工程学报，2008，27(12)：2 387-2 394.(LIN Weiren. A core-based method to determine three-dimensional in-situ stress in deep drilling wells：Anelastic strain recovery technique[J]. Chinese Journal of Rock Mechanics and Engineering，2008，27(12)：2 387-2 394.(in Chinese))
[1]	ZOBACK M D. Reservoir geomechanics[M]. New York：Cambridge University Press，2007：1-505.
[11]	CUI J W，LIN W R，WANG L J，et al. Determination of three-dimensional in situ stresses by anelastic strain recovery in Wenchuan earthquake fault scientific drilling project hole-1 (WFSD-1)[J]. Tectonophysics，2014，619-620：123-132.
[16]	LIN W，KWASNIEWSKI M，IMAMURA T，et al. Determination of threedimensional in-situ stresses from anelastic strain recovery measurement of cores at great depth[J]. Tectonophysics，2006，426(1/2)：221-238.
[19]	ROLPH T C，SHAW J，HARPER T R，et al. Viscous remanent magnetization：a tool for orientation of drill cores[J]// Palaeomagnetic Applications in Hydorcarbon Exploration and Production，Geological Society. London：Special Publication，1995：239-243.
[21]	LIU LF，WANG P，LI Y，et al. Paleozoic reservoir beds and their favorableness in Tazhong Areas of Tarim Basin，Northwest China[J]. Journal of Petroleum Science and Engineering，2009，68：1-18.
[26]	SONE H. Mechanical properties of shale gas reservoir rocks and its relation to the in-situ stress variation observed in shale gas reservoirs[Ph. D. Thesis][D]. Stanford：Stanford University，2012.
[31]	HAIMSONB，LIN W，OKU H，et al. Integrating borehole breakout dimensions，strength criteria，and leak-off test results，to constrain the state of stress across the Chelungpu Fault，Taiwan[J]. Tectonophysics，2010，482：65-72.
[36]	云露，曹自成. 塔里木盆地顺南地区奥陶系油气富集与勘探潜力[J]. 石油与天然气地质，2014，35(6)：788-797.(YUN Lu，CAO Zicheng. Hydrocarbon enticement pattern and exploration potential of the Ordovician in Shunnan area，Tarim Basiin[J]. Oil and Gas Geology，2014，35(6)，788-797.(in Chinese))
[3]	TAN C X，JIN Z J，ZHANG M L，et al. An approach to the present-day three-dimensional(3D) stress field and its application in hydrocarbon migration and accumulation in the Zhangqiang depression，Liaohe field，China[J]. Marine and Petroleum Geology，2001，18：983-994.
[5]	ZOBACK M D，APEL R，BAUMGTIRTNER J，et al. Upper-crustal strength inferred from stress measurements to 6km depth in the KTB borehole[J]. Nature，1993，365：633-635.
[7]	蔡美峰，陈长臻，彭华，等. 万福煤矿深部水压致裂地应力测量[J]. 岩石力学与工程学报，2006，25(5)：1 069-1 074.(CAI Meifeng，CHEN Changzhen，PENG Hua，et al. In-situ stress measurement by hydraulic fracgturing technique in deep position of Wanfu coal mine[J]. Chinese Journal of Rock Mechanics and Engineering，2006，25(5)：1 069-1 074.(in Chinese))
[10]	MATSUKI K，TAKEUCHI K. Three-dimensional in-situ stress determination by anelasticstrain recovery of a rock core[J]. International Journal of Rock Mechanics and Minning Sciences，1993，30：1 019-1 022.
[13]	王连捷，孙东生，林为人，等. 地应力测量的非弹性应变恢复法及应用实例[J]. 地球物理学报，2012，55(5)：1 674-1 681.(WANG Lianjie，SUN Dongsheng，LIN Weiren，et al. Anelastic strainrecovery method to determine in-situ stress and application example[J]. Chinese Journal of Geophysics，2012，55(5)：1 674-1 681.(in Chinese))
[15]	孙东生. 非弹性应变恢复原地应力测量方法的实验研究及应用[博士学位论文][D]. 北京：中国地质科学院，2014.(SUN Dongsheng. Experimental study of anelastic strain recovery in-situ stress measurement methods and its application[Ph. D. Thesis][D]. Beijing：Chinese Academy of Geological Sciences，2014.(in Chinese))
[17]	VOIGHT B. Determination of the virgin state of stress in the vicinity of a borehole from measurements of a partial anelastic strain tensor in drill cores[J]. Felsmechanik und Ingenieurgeologie，1968，6：201-215.
[20]	TAMAKI M，SUZUKI K，FUJII T. Paleocurrent analysis of Pleistocene turbiditesediments in the forearc Basin inferred from anisotropy of magnetic susceptibilityand paleomagnetic data at the gas hydrate production test site in theeastern Nankai Trough[J]. Marine and Petroleum Geology，2015，66：404-417.
[23]	GAO L，LIN W，SUN D，et al. Experimental anelasticstrain recovery compliance of three typical rocks[J]. Rock Mechanics and Rock Engineering，2014，47(6)：1 987-1 995.
[25]	PESKAP，ZOBACK M D. Compressive and tensile failure of inclined well bores and determination of in situ stress and rock strength[J]. Journal of Geophysical Research，1995，100(B7)：12 791-12 811.
[30]	HANDIN J，HAGER R V J R，FRIEDMAN M，et al. Experimental deformation of sedimentary rocks under confining pressure：pore pressure tests[J]. AAPG Bulletin，1963，47：718-755.
[27]	李勇明，郭建春，赵金洲. 超深特低渗储层压裂改造技术关键与对策研究[J]. 钻采工艺，2007，30(2)：56-58.(LI Yongming，GUO Jianchun，ZHAO Jinzhou. The hydraulic fracturing simulation key technology and solution of low permeability reservoir at ultra-depth[J]. Drilling and Production Technology，2007，30(2)：56-58.(in Chinese))
[29]	丁文龙，樊太亮，黄晓波，等. 塔里木盆地塔中地区上奥陶统古构造应力场模拟与裂缝分布预测[J]. 地质通报，2011，30(4)：588-594.(DING Wenlong，FAN Tailiang，HUANG Xiaobo，et al. Upper Ordovician paleo tectonic stress field simulating and fracture distribution forecasting in Tazhong area of Tarim Basin，China[J]. Geological Bulletin of China，2011，30(4)：588-594.(in Chinese))
[32]	BECK R A，BURBANK D W，SERCOMBE W J，et al. Stratigraphic evidence for an early collision between northwest India and Asia[J]. Nature，1995，373：55-58.
[33]	SOBEL E R，DUMITRU T A. Thrusting and exhumation around the margins of the western Tarim Basin during the India-Asiacollision[J]. Journal of Geophysical Research，1997，102：1 043-1 063
[35]	LI Y J，YAN Z，SUN L G，et al. Meso-cenozoic extensional structures in the Northern Tarim Basin，NW China[J]. International Journal of Earth Sciences，2013，102(4)：1 029-1 043.
[37]	何碧竹，乔秀夫，许志琴，等. 塔里木盆地满加尔坳陷及其周缘晚奥陶世古地震记录及其地质意义[J]. 地质学报，2010，35(6)：1 805- 1 817.(HE Bizhu，QIAO Xiufu，XU Zhiqin，et al. Late ordovician paleo-seismic records of the Manjiaer depression and adjacent areas in Tarim Basin，Xinjiang，and its geologic significance[J]. ACTA Geologica Sinica，2010，35(6)，1 805-1 817.(in Chinese))
[38]	AVOUAC J P，TAPPONNIER P，BAI M，et al. Active thrusting and folding along the northern Tien Shan and late Cenozoic rotation relative to Dzungaria and Kazakhstan[J]. Journal of Geophysical Research，1993，98(B4)：6 755-6 804.