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Structural Characteristics and Formation Dynamics: A Review of the Main Sedimentary Basins in the Continent of China

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Acta Geologica Sinica(English Edition) 2016年第4期90卷 1156-1194页

作者： HE Bizhu zheng menglin Institute of Geology Chinese Academy of Geological Sciences Petroleum Exploration and Development Institute Xinjiang Oilfield Company

The formation and evolution of basins in the China continent are closely related to the collages of many blocks and orogenic belts. Based on a large amount of the geological, geophysical, petroleum exploration data and a large number of published research results, the basement constitutions and evolutions of tectonic-sedimentary of sedimentary basins, the main border fault belts and the orogenesis of their peripheries of the basins are analyzed. Especially, the main typical basins in the eight divisions in the continent of China are analyzed in detail, including the Tarim, Ordos, Sichuan, Songliao, Bohai Bay, Junggar, Qiadam and Qiangtang basins. The main five stages of superimposed evolutions processes of basins revealed, which accompanied with the tectonic processes of the Paleo-Asian Ocean, Tethyan and Western Pacific domains. They contained the formations of main Cratons （1850-800 Ma）, developments of marine basins （800-386 Ma）, developments of Marine- continental transition basins and super mantle plumes （386-252 Ma）, amalgamation of China Continent and developments of continental basins （252-205 Ma） and development of the foreland basins in the western and extensional faulted basin in the eastern of China （205~0 Ma）. Therefore, large scale marine sedimentary basins existed in the relatively stable continental blocks of the Proterozoic, developed during the Neoproterozoic to Paleozoic, with the property of the intracontinental cratons and peripheral foreland basins, the multistage superimposing and late reformations of basins. The continental basins developed on the weak or preexisting divisional basements, or the remnant and reformed marine basins in the Meso-Cenozoic, are mainly the continental margins, back-arc basins, retroarc foreland basins, intracontinental rifts and pull-apart basins. The styles and intensity deformation containing the faults, folds and the structural architecture of regional unconformities of the basins, responded to the openings, subd

关键词： sedimentary basin structural architecture superimposed evolution interaction dynamics of basin and orogeny continent of China

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Sequence framework of two different kinds of margins and their response to tectonic activity during the Middle-Late Triassic,Ordos Basin

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Science China Earth Sciences 2007年第z2期50卷 203-216页

作者： YANG MingHui LIU ChiYang zheng menglin LAN ChaoLi TANG Xuan Key Laboratory for Hydrocarbon Accumulation of Education Ministry in China University of Petroleum Basin and Reservoir Research CenterChina University of PetroleumBeijing 102249China State Key Laboratory of Continental Dynamics(Northwest University) Xi'an710069China Exploration&Production Research Institute SINOPECBeijing 100083China School of Engineering of Oil&Gas China University of PetroleumBeijing 102249China School of Energy China University of GeosciencesBeijing 100083China

Two kinds of margin respectively occur in the Ordos Basin during the Middle-Late Triassic(Yanchang Age),one is foreland margin developed under the background of flexural subsidence by thrusting intensively in the southwest margin,and the other is intracratonic basin margin by stable subsidence in northern and central parts of the *** Middle-Late Triassic Yanchang Formation can be divided into four regional third-order sequences,which are separated by gentle angular unconformity or regional erosion surface,made up of lowstand system tract(LST),expanding system tract(EST)and highstand system tract(HST)from lower to upper within a *** there are distinct differences of the sequence framework between the southwest margin and northern and central parts of the *** southwest margin develops heavy conglomerate layer and unconformity as a result of orogeny by thrusting,and the intracratonic basin margin by stable subsidence in the northern and central parts grows aggradational sandstone,conglomerate in fluvio-delta system and parallel *** depositional framework of southwest margin reflects the tectonic evolution from flexural subsidence by thrusting to rebounded *** formation of sequence boundary is related to the resilient uplift and *** sequence stratigraphic framework and depositional system tract configuration in the foreland basin are controlled by structural activity of the fold and thrust belt,and the sequence succession reflects episodic thrusting of the Middle-Late Triassic toward the foreland *** sequence evolution in northern and central parts reflects the depositional succession of fluvio-delta system under intracratonic background,composed of coarse-grained sediment in braided channel deposit at the lower,meandering channel deposit in the middle and fine-grained sediment in the flood plain at the upper,dominated by lake level *** the deposit of the LST in the intracraton basin,accommodation spa

关键词： sequence architecture tectonic response basement structure the Middle-Late Triassic(Yanchang Age) Ordos Basin

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The hydrothermal karstification and its effect on Ordovician carbonate reservoir in Tazhong uplift of Tarim Basin, Northwest China

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Science China Earth Sciences 2007年第z2期50卷 103-113页

作者： WU MaoBing WANG Yi zheng menglin ZHANG WeiBiao LIU ChunYan Institute of Oil Exploration and Development Sinopec Beijing 100083 China Institute of Oil Exploration and Development Sinopec Beijing 100083 China Institute of Oil Exploration and Development Sinopec Beijing 100083 China Institute of Oil Exploration and Development Sinopec Beijing 100083 China Institute of Energy China University of Geosciences Beijing 100083 China

With a detailed study on petrology, mineralogy and geochemistry of some important Ordovician carbonate well core samples in Tazhong uplift of Tarim Basin, the distinguishing symbols of hydrothermal karstification are first put forward as the phenomena of rock hot depigmentation, hot cataclasm and the appearance of typical hydrothermal minerals such as fluorite, barite, pyrite, quartz and sphalerite. The main homogenization temperatures of primary fluid inclusions in fluorite are from 260 to 310℃, indicating the temperature of hydrothermal fluid. The fluid affected the dissolved rocks and showed typical geochemistry features with low contents of Na and Mg, and high contents of Fe, Mn and Si. The ratio of 3He/4He is 0.02Ra, indicating the fluid from the typical continental crust. The hydrothermal fluid karstification pattern may be described as follows: the hot fluid is from the Permian magma, containing dissolving ingredients of CO2 and H2S, and shifts along fault, ruptures and unconformity, and dissolves the surrounding carbonates while it flows. The mechanism of hydrothermal karstification is that the mixture of two or more fluids, which have different ion intensity and pH values, becomes a new unsaturated fluid to carbonates. The hydrothermal karstification is an important process to form hypo-dissolved pinholes in Ordovician carbonates of Tazhong uplift of Tarim Basin, and the forming of hydrothermal minerals also has favorable influence on carbonate reservoirs.

关键词： hydrothermal karstification, hydrothermal mineral, carbonate reservoir, Ordovician, Tazhong region

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Water pollution footprints induced by industrial import and export in China

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Chinese Journal of Population,Resources and Environment 2018年第2期16卷 149-158页

作者： Yutao Lei Li Su menglin zheng School of Economics and Commerce South China University of Technology

With the rapid development of foreign trade in China, industrial import and export has been an absolute subject in recent years. The huge trade surplus of import and export trade of industrial products brings not only high profits, but also pollution costs as well. Based on the concept of water pollution footprints(WPFs), this study applies the input-output method and calculates pollutant-producing coefficients of 20 major industrial sectors in China and investigates the WPFs caused by the import and export trades of these industrial sectors. The research results show that WPF resulting from exports exceeds that of imports from 2011 to 2015 in China. The net inflow of pollution footprint is mainly from paper mills, printing and stationery manufacturing, and textile industry; whereas a great number of WPFs are transferred to other countries by these sectors,such as metal mining and dressing industry and oil and natural gas exploitation industry.

关键词： Industrial products import and export trade pollution footprint

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Characteristics and Main Controlling Factors of Tight Oil Reservoir in the Jimsar Sag of Junggar Basin

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Acta Geologica Sinica(English Edition) 2015年第A01期89卷 182-183页

作者： BAO Haijuan HE Wenjun FEI Liying JIA Xiyu zheng menglin YANG Haibo GGUO Xuguang Petroleum Exploration and Development Institute Xinjiang Oilfield Company

1 Introduction Jimsar sag covers about 1278 km2 in the south of the eastern uplift of Junggar basin. It is a half graben depression area in which the west, south and north is controlled by faults （Fig. 1）, and is tilting uplift to the east. It deposited Permian, Triassic, Jurassic, the Cretaceous and Cenozoic strata chronologically. The thickness of Lucaogou Formation is about 200 m to 350 m, it is the source rocks in the area, and is also a typical self- generating and self-preserving tight oil reservoir trapped strata.

关键词： PETROLEUM reserves BASINS (Geology) POROSITY RESERVOIRS BIOACCUMULATION CHINA

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Tectonic and climatic controls on the formation of alkaline lake during the Permian Fengcheng Formation in the Mahu Sag， northwestern Junggar Basin， China

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Journal of Earth Science 2024年

作者： Yong Tang Bao Zhang Detian Yan Liwei Zhang menglin zheng Lei Zhang Xiaosong Wei Yu Bai Exploration and Development Institute， Xinjiang Oilfield Company Petro-China Exploration and Development Research Institute SINOPEC Jianghan Oilfield Company Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education， China University of Geosciences

Alkaline lakes hold significant biological， environmental， and economic importance， yet research on their deep-time formation remains limited. This study examines the sedimentary and evolutionary processes of the Permian Fengcheng Formation alkaline lake in the Mahu Sag， Junggar Basin， using seismic， well-log， core， mineralogical， and geochemical data. Results indicate that alkaline mineral formation primarily occurred in rift climax systems， where fan delta plains and lacustrine environments coexisted. Nahcolite (NaHCO3) formed as leafy crystals through evaporation on the outer fan margins， with nucleation at the bottom. Trona (Na2CO3·NaHCO3·2H2O) precipitated as raft-shaped crystals from saline water. Dark sediments interbedded with shortite (Ca2Na2(CO3)3) formed in deepwater environments under arid， cold conditions. The rift expansion facilitated evaporite deposition， and hydrothermal fluids cofntributed alkaline substances. Late Paleozoic glaciation increased chemical weathering， enhancing lake alkalinity， while arid conditions favored evaporite formation. An impermeable basement and semi-enclosed hydrology were critical for alkaline lake development. This study sheds light on the conditions for ancient sodium carbonate evaporite formation and provides insights into the sedimentary evolution of similar tectonic and climatic lake basins， offering a foundation for hydrocarbon exploration.

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塔里木盆地台盆区火山作用对有机质演化的影响

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石油学报 2007年第6期28卷 17-20页

作者：周波金之钧王毅郑孟林中国石化石油勘探开发研究院

对塔里木盆地台盆区中1井和中11井的有机质成熟度演化规律分析发现,同处于台盆区的2口探井距离仅约13km,地层演化和构造特征相似,其有机质演化规律却截然不同。对其岩性特征和有机质演化的对比表明,发生有机质演化突变之处正是火山物质... 详细信息

对塔里木盆地台盆区中1井和中11井的有机质成熟度演化规律分析发现,同处于台盆区的2口探井距离仅约13km,地层演化和构造特征相似,其有机质演化规律却截然不同。对其岩性特征和有机质演化的对比表明,发生有机质演化突变之处正是火山物质开始增多的地方,这说明火山作用的存在导致了有机质演化规律的突变。这2口井也可以作为火山作用对有机质演化规律产生影响的范例。

关键词：塔里木盆地有机质演化火山作用火山物质凝灰岩含量

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POSSIBLE EXTENDING OF BANGONGHU-DINGQING SUTURE AND ITS GEOLOGICAL RELEVATIONS

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地学前缘 2000年第S1期7卷 162-163页

作者： Liu Chiyang,Lu Bing, zheng menglin,Lai Shaochong,Wang Dingyi,Ren Zhanli,Chen Gang(Northwestern University,Xi’an 710069,China)

Basic features Bangonghu—Dingqing Suture is the medial and western segment of the Bangonghu—Nujiang Suture which many researchers called as ,and it is often regarded as the Qiangtang Massif boundary line in the northern side and the Lasa (Gangdisi) Massif in the souther. The era of the ophiolites spreading along the Bangonghu\|Dingqing suture include every period of the whole Jurassic, and the spreading of the ophiolites has distinct segmentation. From west to east there are Ritu segment,Gaize segment,Dongqiao segment and Dingqing *** the Gaize segment and Dongqiao one ,that is ,between the E89°and E86°40′,no ophiolites are discovered in the *** data shows that the magnetic field of this segment is quite gentle,there are no difference from its adjacent northern and southern sides. When its east adjacent segment extends into this segment, the high areomagnetic anomaly belt corresponding to of the Dongqiao ophiolite disappear abruptly. Apparently,it is impossible for the ophiolites to develop in such a deep crust of the same segment.

关键词： Bangonghu—Dingqing suture Qiangtang massif chashang segment transform fault tectonic segmentation

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中国西北地区沉积盆地发育的区域构造格局与演化

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地学前缘 2015年第3期22卷 227-240页

作者：何治亮高山林郑孟林中国石化石油勘探开发研究院北京100083 中国石油新疆油田分公司勘探开发研究院新疆克拉玛依834000

中国西北地区是不同地质时期多个全球性大地构造单元的组成部分,具有南北分带、东西分区的构造特征,经历了中、新元古代—古生代期间地壳增生、洋-陆转换、板块开-合旋回、晚二叠世以来盆地的叠加改造和新生代印度与欧亚板块碰撞远源效... 详细信息

中国西北地区是不同地质时期多个全球性大地构造单元的组成部分,具有南北分带、东西分区的构造特征,经历了中、新元古代—古生代期间地壳增生、洋-陆转换、板块开-合旋回、晚二叠世以来盆地的叠加改造和新生代印度与欧亚板块碰撞远源效应等长期演化过程,具有明显的阶段性。研究表明,现今盆地多位于具有一定规模的经过前震旦系不断增生作用所形成的陆块基底之上,塔里木盆地塔中、塔北、塔东北地区基底可能以古元古界为主,而巴楚地区则以晋宁期的变质基底为主。准噶尔盆地前震旦纪存在多个独立发育的块体,古生代总体具有多岛洋的性质。柴达木盆地、河西走廊及邻区的诸多中小型盆地的基底主要为中元古代形成。敦煌盆地、北山地区众多中小型盆地坐落在中小地块或者古生代活动陆缘的岛弧之上。西北地区早古生代经历了一个完整的板块开-合旋回,但不同地区有不同表现方式。北疆地区至少存在寒武纪—早奥陶世、志留纪和泥盆纪3个主要时期的蛇绿岩,反映了在早、晚古生代各存在一定规模的洋盆。在不同带的早古生代洋盆具有不同的闭合时间。塔里木盆地周缘南天山洋、西昆仑洋及阿尔金、祁连、东昆仑、北山地区早古生代洋盆的发育时间为寒武纪早期,经过了中、晚寒武世到早奥陶世早期洋盆的扩张,早奥陶世晚期构造应力场转为挤压体制。志留纪中晚期至早泥盆世,西北地区存在全区性的板块拼合与碰撞以及不同程度的变形变质过程。西北地区晚古生代又经历了一个完整的板块开-合旋回,天山全区、准噶尔南部、东西两侧分别进入碰撞后新的大规模的伸展阶段,均形成了有限洋盆,其时代略有差别,上、下石炭统之间可能存在构造转换。塔西南地区早石炭世伸展作用形成了晚古生代的西昆仑洋和陆缘裂陷盆地,中二叠世康西瓦—苏巴什洋盆向北侧俯冲消减,发生于中、晚二叠世之间的海西晚期构造运动是西北地区具有重大变革意义的一次构造运动。晚二叠世—新生代是西部地区构造格局大的调整与定型时期,在总体表现为多板块拼合后的宏观背景下,经历了多期幕式挤压与伸展交替的构造演化过程,并不是以往所简单认为的各种前陆盆地的组合,晚期均受到了青藏高原快速隆升所导致的远源碰撞作用的强烈改造。构造格局的差异性和演化的阶段性使西北不同地区、不同时期盆地发育和叠加组合方式差异很大,油气地质条件的明显不同,油气资源丰度差别很大。

关键词：中国西北地区区域构造格局构造演化盆地基底板块开-合旋回复合叠加盆地

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塔里木盆地沙雅隆起形成演化与油气分布规律

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大地构造与成矿学 2013年第3期37卷 398-409页

作者：谢大庆郑孟林蒋华山郭忻中国石化西北油田分公司研究院新疆乌鲁木齐830011 中国石化石油勘探开发研究院北京100083

沙雅隆起是塔里木盆地重要的油气聚集单元,有关隆起结构、演化及其对油气藏控制的认识始终存在争议。本文通过全区钻井资料的分析和地震资料解释,进行了地质编图,对复杂油气藏分布规律和控制因素进行了解剖,明确了关键构造事件和隆起的... 详细信息

沙雅隆起是塔里木盆地重要的油气聚集单元,有关隆起结构、演化及其对油气藏控制的认识始终存在争议。本文通过全区钻井资料的分析和地震资料解释,进行了地质编图,对复杂油气藏分布规律和控制因素进行了解剖,明确了关键构造事件和隆起的演化特征。研究证实,隆起经历了寒武纪-奥陶纪沉积古隆起、志留纪-白垩纪构造古隆起和新生代埋藏古隆起三大演化阶段,发生了多期构造事件,形成了多个不整合面。志留系沉积前的构造事件导致了雅克拉断凸的形成,断凸区成为志留系的物源区。东河砂岩-石炭系沉积前的构造事件在隆起南部形成了英买力、哈拉哈唐、阿克库勒、草湖等背、向斜,形成了凹、凸结构,并形成了近南北向、北东向、北西向和东西向的断裂。古近纪的弱伸展-剪切作用导致了老断层的重新活动,在盆地浅层形成了一系列雁列构造,使隆起复杂化。新近纪以来的翘倾作用导致了隆起区三叠系以来的地层向北倾伏。隆起的南北分带和纵向分层特征控制了油气的分布,形成了两个油气聚集带、一个油气聚集区。纵向上形成了深部与碳酸盐岩地层相关油气藏和浅层与断裂、低幅度构造、地层不整合、岩性等相关的油气藏。浅层油气藏一般位于深层碳酸盐岩大型油气藏的上部,为次生油气藏。油气藏的形成除了受烃源岩分布、断裂、褶皱、隆起、不整合等因素控制外,碳酸盐岩岩性的溶蚀性差异也导致了油气成藏的复杂性。

关键词：沙雅隆起形成演化不整合油气分布控制因素

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