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| 1 | 塔里木克拉通基底古隆起构造-热事件及其结构与演化显示文摘通过盆地内部锆石U-Pb测年分析表明,塔里木克拉通基底存在2950~3100Ma、2100~2400Ma、1900~2000Ma、1300~1600Ma、900~950Ma、700~800Ma、540~560Ma、400~500Ma和270~290Ma等9期构造-热事件。中央航磁异常带井下花岗岩锆石SHRIMPU-Pb年龄测定发现1908.2±8.6Ma前寒武纪基底,表明盆地内部可能存在古元古代构造-热事件形成的古老花岗岩基底。结合新的地质与地球物理资料综合分析,塔里木盆地前寒武纪具有不同年代、不同类型的基底结构,北部为中-新元古代中浅变质岩基底、中部为古元古代花岗岩基底、南部为新元古代早-中期岩浆岩与变质岩基底、东南部为遭受早志留纪区域变质改造的变质岩基底。井震结合发现塔里木盆地寒武系/前寒武系发育广泛分布的大型不整合,形成塔北与塔南两大前寒武纪基底古隆起,可能与550Ma'泛非运动'相关。塔里木盆地基底古隆起主要经历5期演化,古元古代中期形成克拉通化基底,新元古代早期形成统一的变质结晶基底,寒武纪沉积前两大基底古隆起形成,加里东晚期五大基底古隆起基本定型,海西期以来发生局部调整改造。 | 邬光辉 李浩武 徐彦龙 苏文 陈志勇 张宝收 | 2012 | 岩石学报2012，28，8： | 77 |
| 2 | 塔里木盆地走滑带碳酸盐岩断裂相特征及其与油气关系显示文摘通过露头与井下资料的综合分析,塔里木盆地奥陶系碳酸盐岩走滑断裂带断裂相具有多样性,根据内部构造发育程度可以分为断层核发育、断层核欠发育两类。露头走滑带断层核部以裂缝带、透镜体、滑动面等断裂相发育为特征,断裂边缘的破碎带发育裂缝带、变形带。裂缝带主要分布在断层核附近50m的破碎带内,裂缝多开启,渗流性好。断裂核部透镜体发育,在破碎带也有分布,破碎角砾组合的透镜体多致密。滑动面具有平直截切型、渐变条带型等两种类型,多为开启的半充填活动面。变形带多为方解石与碎裂岩充填,破碎带局部部位裂缝与溶蚀作用较发育。利用地震剖面、构造图、相干图等资料可以判识塔里木盆地内部奥陶系碳酸盐岩走滑断裂相的特征及其发育程度,沿走滑断裂带走向上断裂相具有分段性与差异性,根据渗流性可以定性区分高渗透相、致密相区。沿断裂带高渗透相区是碳酸盐岩缝洞体储层发育的有利部位。断裂相的横向变化造成油气分布的区段性,形成高渗透相输导模式、致密相遮挡模式等两类成藏模式。走滑断裂带碳酸盐岩断裂相的特征及其控藏作用对油气勘探开发储层建模具有重要意义。 | 邬光辉 陈志勇 曲泰来 王春和 李浩武 朱海燕 | 2012 | 地质学报2012，86，2： | 55 |
| 3 | 塔里木盆地麦盖提斜坡奥陶系风化壳成藏条件显示文摘基于地震、钻井资料综合研究,分析塔里木盆地麦盖提斜坡及其周缘古隆起背景上奥陶系风化壳特征及其储集层发育主控因素,探讨该区油气分布规律与勘探方向。区域构造成图与构造解析表明,麦盖提斜坡及其周缘发育塔里木盆地最大规模的奥陶系碳酸盐岩风化壳,与上覆志留系/石炭系泥岩形成优质储盖组合。奥陶系碳酸盐岩历经多期大型岩溶作用,以受古岩溶地貌、构造作用与岩性控制的小型缝洞体储集层为主。已有钻探多位于北部岩溶缓坡—洼地,岩溶作用较弱、充填严重,据古地貌分析与储集层预测,南部岩溶斜坡区储集层应更发育。构造演化与生烃演化史综合分析表明,碳酸盐岩古隆起演化与变迁控制了油气的运聚与分布,具有晚海西期成油、喜马拉雅晚期调整与原油裂解气再成藏的两期充注史。古隆起东西两端的玛南、麦西斜坡区长期位于油气聚集与调整的有利部位,具备形成大面积碳酸盐岩缝洞型岩性油气藏的地质条件,是塔里木盆地碳酸盐岩油气勘探的有利接替领域。 | 邬光辉 李洪辉 张立平 王成林 周波 | 2012 | 石油勘探与开发2012，39，2： | 38 |
| 4 | Reservoir characteristics,formation mechanisms and petroleum exploration potential of volcanic rocks in China显示文摘Characterized by complex lithology and strong heterogeneity, volcanic reservoirs in China developed three reservoir space types: primary pores, secondary pores and fractures. The formation of reservoir space went through the cooling and solidification stage(including blast fragmentation, crystallization differentiation and solidification)and the epidiagenesis stage(including metasomatism, filling, weathering and leaching, formation fluid dissolution and tectonism). Primary pores were formed at the solidification stage, which laid the foundation for the development and transformation of effective reservoirs. Secondary pores were formed at the epidiagenesis stage, with key factors as weathering and leaching, formation fluid dissolution and tectonism. In China, Mesozoic–Cenozoicvolcanic rocks developed in the Songliao Basin and Bohai Bay Basin in the east and Late Paleozoic volcanic rocks developed in the Junggar Basin, Santanghu Basin and Tarim Basin in the west. There are primary volcanic reservoirs and secondary volcanic reservoirs in these volcanic rocks, which have good accumulation conditions and great exploration potential. | Zhi-Guo Mao Ru-Kai Zhu Jing-Lan Luo Jing-Hong Wang Zhan-Hai Du Ling Su Shao-Min Zhang | 2015 | Petroleum Science2015，12，1： | 12 |
| 5 | 碳酸盐岩断层破碎带构造成岩作用——以塔中Ⅰ号断裂带为例显示文摘多旋回叠合盆地断层具有异常复杂的构造变形与成岩演变,跨学科结合的构造成岩作用研究为断层破碎带演变机制与流体-岩石作用分析提供了新思路。结合塔中Ⅰ号断裂带构造解析和地化资料分析,探讨古老碳酸盐岩断层破碎带构造成岩作用的特殊性。结果表明,塔中Ⅰ号断裂带上奥陶统台缘带碳酸盐岩断层破碎带发育多类、多期构造成岩作用,明显不同于围岩。断层破碎带宽度高达2~4km,裂缝类型多样、纵横向变化大、开启程度较高。沿断裂带压实作用较弱且有差异,发现有碳酸盐岩压实变形带发育,并有后期裂缝与溶蚀作用形成的局部高渗透带。断层破碎带观测到多期压溶低角度缝合线与高角度构造缝合线,部分具有渗透性。多达4~5期不同类型胶结作用沿裂缝带发育,大气淡水胶结较多,胶结程度相对较弱。准同生期大气淡水溶蚀与局部风化壳岩溶主要沿断层破碎带发育,而且埋藏溶蚀作用较强,发育大型缝洞体与溶蚀孔洞。构造成岩作用揭示塔中Ⅰ号断裂带东段上奥陶统碳酸盐岩断层破碎带经历断裂萌芽期-形成期-定型期-复活扩张期-局部开启期等5期演变,不同演化期构造成岩作用有明显差异。构造成岩作用的多期差异活动是造成古老碳酸盐岩断层破碎带复杂性的重要因素。 | 张丽娟 邬光辉 何曙 佘治成 潘杨勇 | 2016 | 岩石学报2016，32，3： | 12 |
| 6 | Origin of the unusually high dibenzothiophene concentrations in Lower Ordovician oils from the Tazhong Uplift,Tarim Basin,China显示文摘The origin of the unusually high dibenzothiophene (DBT) concentrations in Lower Ordovician oils from the Tazhong Uplift,Tarim Basin was studied by Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR MS).The most abundant sulfur compounds in the oils are S 1 species with doublebond equivalent (DBE) values of 1-19 and 11-48 carbon atoms.The range of the number of carbon atoms in the sulfur compounds detected by the FT-ICR MS (S 1 species with DBE=9) is about ten times larger than that for sulfur compounds detected by GC/MS (DBTs).This suggests that FT-ICR MS is a much better approach than GC/MS for characterization of DBTs in crude oils.The abundance of S 1 species with DBE=1-8 decreased with increasing thermal maturity,while the abundance of S 1 species with DBE=9 (primarily DBTs) increased.Therefore,thermal maturity is an important factor in the formation of oils with high DBT concentrations.Unusually high abundances of S 1 species with low DBE values (1-8),which include sulfide,thiophene and benzothiophene,were observed in several oils,especially the TZ83 (O 1) oil with high or very high thermal maturity.Thermochemical sulfate reduction (TSR) was thought to be the reason for the high abundance of these low DBE compounds in deep reservoirs,and thermochemical sulfate reduction could affect the distribution and composition of DBTs in the oils.According to the results of FT-ICR MS analysis,there are no signs that TSR is occurring or has occurred recently for most of the Lower Ordovician oils. | Li Sumei Pang Xiongqi Shi Quan Zhang Baoshou Zhang Haizu Pan Na Zhao Ming | 2011 | Petroleum Science2011，8，4： | 9 |
| 7 | 塔里木盆地塔中Ⅰ号构造带分段变形的运动学特征与成因探讨显示文摘塔里木盆地塔中Ⅰ号构造带在构造样式、活动强度等方面表现出明显的分段性,但分段变形的运动学特征与成因仍不够明确,需要开展进一步研究。本文利用二维、三维地震资料,通过精细构造解析、运动学参数统计、活动期次厘定等手段,研究了塔中Ⅰ号构造带的几何学、运动学特征,分析其分段变形机制,并讨论了分段控制因素。研究表明:以中古15井与中古21井位置为界,塔中Ⅰ号构造带构造样式、运动学特征主要呈三段的特点,西段主要活动机制是断裂短距离滑动逆冲和地层旋转变形,同一层位的落差/垂直断距(H/h)值最大;中段为断裂沿走向滑动,H/h值约为1;东段为断裂长距离滑动逆冲和强烈褶皱,H/h值介于二者之间。活动机制的差异导致各段构造样式分别为基底卷入逆冲断裂控制的断层传播褶皱、走滑断裂发育的断控坡折、逆冲断裂强烈活动控制的断块褶皱,且活动强度呈现东段最大、西段次之、中段较小的特点。两大造山带分期活动是塔中Ⅰ号构造带分段变形的发育背景,基底结构与先存断裂是造成分段的主控因素,NE向走滑断裂调节塔中Ⅰ号构造带差异逆冲变形,并作为伴生断裂发育。 | 张仲培 王璐瑶 邓尚 魏华动 张继标 | 2020 | 地质论评2020，66，4： | 5 |
| 8 | 碳酸盐岩变形带特征及其与油气关系——以塔里木盆地下古生界为例显示文摘深入了解变形带的差异性对碳酸盐岩储层渗流作用与油气勘探开发研究具有重要意义。通过野外露头、井下岩心的宏观与微观特征分析,发现塔里木盆地下古生界碳酸盐岩变形带发育,存在压实变形带、剪切变形带和膨胀变形带等3类成因变形带。根据变形带的发育演化特征可以进一步划分为8种类型:压实变形带又可分为解聚压实变形带、碎裂压实变形带和压溶压实变形带3种类型;解聚剪切变形带、碎裂剪切变形带和胶结剪切变形带则是3种常见的剪切变形带;膨胀变形带包括碎裂膨胀变形带和胶结膨胀变形带。不同类型变形带特征各异,以解聚压实变形带与碎裂剪切变形带最发育,各类变形带呈现从解聚型向剪切型和胶结型演变的趋势。不同于碎屑岩变形带渗透性急剧降低,塔里木盆地碳酸盐岩变形带的物性与围岩差别较小,不同次级类型变形带渗流特征不同,局部孔隙发育,并影响油气储层非均质性。受控于溶蚀、破裂与白云石化等三种后期改造作用,塔里木盆地下古生界碳酸盐岩发育高渗透变形带,可能形成有效渗流通道。 | 邬光辉 陈志勇 郭群英 | 2014 | 大地构造与成矿学2014，38，3： | 5 |
| 9 | Dynamic Processes of the Paleozoic Tarim Basin and Its Significance for Hydrocarbon Accumulation——A Review and Discussion显示文摘The structural framework and evolution processes of the giant superimposed Tarim basin in Paleozoic Era are controlled by three main factors:(1) features and structures of the basin basement;(2) deep mantle dynamics process(such as the Sinian rifting and the Permian plume-related magmatic activities);(3) the powerful regional compressional or compresso-shear stress regime generated by the orogenic movement from surrounding regions.The latter of which occurring in multiple episodes is the most important factor for the Paleozoic Tarim basin evolution.Under the above tectonic background,the underlying lithosphere of the Tarim basin had been flexed,and then the upper crust was folded.The paleo-uplifts(e.g.,Tabei(塔北) and Tazhong(塔中)) and depressions occurred in both of the flexural and folding processes,which are different with the models of foreland basin in stable and large cratons in the world.During the early evolution stage in Cambrian-Early Ordovician,low-relief paleo-uplifts,and open carbonate platforms formed in center area,while during the Late Ordovician compressional tectonic regime,the belted uplifts and restricted platforms formed in the contemporaneous folding processes.Denudated stages occurred during the strong tectonic events marked by the unconformities and karstified weathered crusts formed on platforms.All the discovered giant-middle oilfields are closely related to the paleo-uplift and karstified crust evolution.There are two main types of oil reservoir:paleo-karst type and reef-bank type on the carbonate platform in paleo-uplift areas.In Permian,plume-related massive magmatic activities led to geo-temperature increase and the regional uplifting in this basin,ending the marine deposit filling sequences and starting the formation of terrestrial deposits-dominated sequences.With abundant supply from giant hydrocarbon generation depressions,the most important oil fields formed in Tabei and Tazhong areas.To reveal the multi-stage evolution processes and the structural framework of the paleo-uplifts may be helpful for the prediction of new hydrocarbon domains.The integrated study on coupling relationship between the basin and surrounding orogens can provide an important approach for the superimposed basin dynamic research. | 李思田 任建业 邢凤存 刘占红 李红谊 陈强路 李祯 | 2012 | Journal of Earth Science2012，23，4： | 3 |
| 10 | 塔中隆起深层构造样式及其成因探讨显示文摘塔中隆起是研究塔里木盆地下古生界构造样式的良好窗口。基于对塔中隆起三维地震工区的精细解析,依据断裂期次匹配关系及断裂组合方式,可将塔中隆起三维地震工区分为3个构造样式区,即西部单冲推覆构造区、中部盐上盖层滑脱构造区及东部继承性冲断构造区。塔中隆起三维地震工区在整体上具有西部构造区变形弱,东部构造变形强的特征。最西部的单冲推覆构造区构造样式以简单的单冲推覆构造为主,且推覆构造主要集中在塔中I号断裂带,同时盐下深部地层还保存有早期的正断裂。中部的盐上盖层滑脱构造区构造样式以挤压型盐上盖层滑脱为特征,且向东滑脱幅度明显增大,盐下深部早期正断裂大多发生反转。东部继承性冲断构造区发育大量的基底卷入型逆冲断层,断层多刺穿盐层,且逆冲断层多沿早期正断裂发育。区域挤压应力的差异、膏盐岩分布的差异及先存断裂的影响是导致工区内不同区域构造特征差异的主要因素。 | 王洪浩 李江海 孙唯童 程雅琳 | 2016 | 天然气技术与经济2016，10，1： | 2 |
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