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基于弹性板模型的塔里木盆地北部新生代沉降模拟:对南天山隆升的启示

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地学前缘 2024年第4期31卷 340-353页

作者：陈昌锦程晓敢林秀斌李丰田禾丰屈梦雪孙思瑶浙江大学地球科学学院浙江省地学大数据与地球深部资源重点实验室浙江杭州310058 教育部含油气盆地构造研究中心浙江杭州310058

在印度-欧亚板块碰撞远程效应影响下,天山造山带在新生代活化隆升,与其南缘相邻的塔里木盆地北部发生挠曲沉降并沉积了巨厚的新生代地层,该巨厚新生代地层和造山沉积地层为本文进一步探究南天山隆升过程提供了关键的沉积记录。本文采用... 详细信息

在印度-欧亚板块碰撞远程效应影响下,天山造山带在新生代活化隆升,与其南缘相邻的塔里木盆地北部发生挠曲沉降并沉积了巨厚的新生代地层,该巨厚新生代地层和造山沉积地层为本文进一步探究南天山隆升过程提供了关键的沉积记录。本文采用有限弹性板数值模拟的方法,对盆地新生代不同时期基底沉降剖面分别进行建模研究。结果表明:盆地沉降受沉积负载和构造负载共同控制,66~<5.3 Ma期间沉积负载对盆地沉降的贡献量小于或等于构造负载的贡献量;约5.3 Ma至今沉积负载对盆地沉降的贡献量远大于构造负载。南天山构造负载变化速率表现为66~<26.3 Ma缓慢增长;26.3~<5.3 Ma南天山稳定增长;约5.3 Ma至今南天山造山带构造负载高度快速增长。基于对盆地沉降过程的分析,限制南天山新生代初始隆升时间为古近纪,其相对海拔高度从400 m增长到2 500 m;虽然在约5.3 Ma至今南天山相对海拔高度保持稳定,但构造负载高度仍在增加,这可能是盆地俯冲作用的加剧在一定程度上抑制了造山带平均海拔高度的增长,进而导致南天山的侵蚀和隆升达到相对平衡。

关键词：南天山塔里木盆地北部有限弹性板模拟沉降过程初始隆升

The Ductile Deformation Characteristics of Caledonian Intracontinental Orogeny in the Northeastern Jiangshan-Shaoxing Tectonic Zone:Insights from Magnetic Fabric Study and Its Geodynamic Implication

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Acta Geologica Sinica(English Edition) 2016年第1期90卷 75-87页

作者： GONG Genhui CHEN Hanlin WANG Fang lin xiubin MENG Lifeng Departement of Earth Sciences Zhejiang University Research Center of Structures in Oil and Gas Bearing Basin Ministry of Education

The Jiangshan-Shaoxing tectonic zone was the northeastern boundary between the Yangtze Block and the Cathaysia Block during the Neoproterozoic and was an intracontinental orogenic belt during late of the early Paleozoic. In this tectonic zone, there develops a lot of mylonite underwent strong ductile deformation and schist, gneiss, and amphibolite with medium and high grade metamorphism which was formed during the late of early Paleozoic. The research of geometry and kinematic of ductile deformation in Jiangshan-Shaoxing tectonic zone is very important to reveal the tectonic process of intracontinental orogeny. This paper uses the anisotropy of magnetic susceptibility （AMS） to determine the ductile deformation geometry and kinematic of Jiangshan-Shaoxing tectonic zone combing with the field survey. In this study, 190 specimens of 19 locations and 221 specimens of 23 locations from Wangjiazhai section and Lipu-Sizhai section were analyzed. The magnetic foliation over magnetic lineation in both Wangjiazhai and Lipu-Sizhai sections together with the field observations indicated a compressional deformation pattern. 3 and 4 strong ductile deformation zones can be established in the Wangjiazhai section and the Lipu-Sizhai section, respectively. According to the magnetic fabric and petro-fabric studies, the Northeastern Jiangshan-Shaoxing tectonic zone suffered two kinds of deformation patterns during the late early Paleozoic, i.e., the thrusting deformation followed by sinistral shear deformation.

关键词： magnetic fabric ductile deformation deformation intensity deformation pattern Jiangshan-Shaoxing tectonic zone

Conceptual models for fracturing in fault related folds

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Mining Science and Technology 2010年第1期20卷 103-108页

作者： lin xiubin CHEN Hanlin CHENG Xiaogan SHEN Zhongyan YANG Shufeng XIAO Ancheng Department of Earth Sciences Zhejiang University Hangzhou 310027 China Research Center for the Structures in Oil and Gas Bearing Basin Ministry of Education Hangzhou 310027 China

Fault related folds and fractures, which always improve reservoirs and trap capacity, especially in the oil and gas fields in western China, are of extreme importance for oil and gas exploration. Based on four assumptions and fault related fold theory, we propose four conceptual models for fracturing in fault related folds, i.e., a simple-step parallel fault bend anticline, a simple-step parallel fault propagation anticline, a multiple-bend fault-bend fold and a break-forward imbricate. Fracture conditions depend on structural evolution and specific site conditions. A case study of the Kulongshan Anticline in the Jiuquan Basin shows that our conceptual models match reality data very well.

关键词： fracturing fault related fold oil and gas exploration

Surface Processes Driving Intracontinental Basin Subsidence in the Context of India–Eurasia Collision:Evidence from Flexural Subsidence Modeling of the Cenozoic Southern Tarim Basin along the West Kunlun Foreland,NW Tibetan Plateau

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Acta Geologica Sinica(English Edition) 2023年第6期97卷 1778-1786页

作者： HUANG Hao lin xiubin AN Kaixuan ZHANG Yuqing CHEN Hanlin CHENG Xiaogan LI Chunyang Key Laboratory of Geoscience Big Data and Deep Resources of Zhejiang Province School of Earth SciencesZhejiang UniversityHangzhou 310027China Research Center for Structures in Oil and Gas-Bearing Basins Ministry of EducationHangzhou 310027China Research Institute of Petroleum Exploration and Development PetroChinaBeijing 100083China Research Institute of Petroleum Exploration and Development Sinopec Southwest Oil and Gas CompanyChengdu 610041China

The India–Eurasia collision has produced a number of Cenozoic deep intracontinental basins,which bear important information for revealing the far-afield responses to the remote *** their significance,their subsiding mechanism remains the subject of debate,with end-member models attributing it to either orogenic or sedimentary *** this study,we conduct flexural subsidence modeling with a two-dimensional finite elastic plate model on the Hotan-Mazatagh section along the southern Tarim Basin,which defines a key region in the foreland of the West Kunlun Orogen,along the NW margin of the Tibetan *** modeling results indicate that the orogenic load of West Kunlun triggers the southern Tarim Basin to subside by up to less than ~6 km,with its impact weakening towards the basin interiors until ~230 km north from the Karakax *** sedimentary load,consisting of Cenozoic strata,forces the basin to subside by ~2 to~7 *** combination with the retreat of the proto-Paratethys Sea and the paleogeographic reorganization of the Tarim Basin,we propose that surface processes,in particular a shift from an exorheic to an endorheic drainage system associated with the consequent thick sedimentary load,played a decisive role in forming deep intracontinental basins in the context of the India-Eurasia collision.

关键词： flexural subsidence modeling India-Eurasia collision West Kunlun Tarim Basin Northwest Tibetan Plateau

The Exhumation History of North Qaidam Thrust Belt Constrained by Apatite Fission Track Thermochronology:Implication for the Evolution of the Tibetan Plateau

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Acta Geologica Sinica(English Edition) 2016年第3期90卷 870-883页

作者： CHENG Xiaogan lin xiubin WU Lei CHEN Hanlin XIAO Ancheng GONG Junfeng ZHANG Fengqi YANG Shufeng School of Earth Sciences Zhejiang UniversityHangzhou 310027ZhejiangChina Research Center for Structures in Oil-and Gas-Bearing Basins Ministry of EducationHangzhou 310027ZhejiangChina

Determining the spatio-temporal distribution of the deformation tied to the India-Eurasian convergence and the impact of pre-existing weaknesses on the Cenozoic crustal deformation is significant for understanding how the convergence between India and Eurasia contributed to the development of the Tibetan Plateau. The exhumation history of the northeastern Tibetan Plateau was addressed in this research using a new apatite fission track （AFT） study in the North Qaidam thrust belt （NQTB）. Three granite samples collected from the Qaidam Shan pluton in the north tied to the Qaidam Shan thrust, with AFT ages clustering in the Eocene to Miocene. The other thirteen samples obtained from the Luliang Shan and Yuka plutons in the south related to the Luliang Shan thrust and they have showed predominantly the Cretaceous AFT ages. Related thermal history modeling based on grain ages and track lengths indicates rapid cooling events during the Eocene-early Oligocene and since late Miocene within the Qaidam Shan, in contrast to those in the Cretaceous and since the Oligocene-Miocene in the Luliang Shan and Yuka region. The results, combined with published the Cretaceous thermochronological ages in the Qaidam Shan region, suggest that the NQTB had undergo rapid exhumation during the accretions along the southern Asian Andean-type margin prior to the India-Eurasian collision. The Cenozoic deformation initially took place in the North Qaidam thrust belt by the Eocene, which is consistent with the recent claim that the deformation of the northeastern Tibetan Plateau initiated in the Eocene as a response to continental collision between India and Eurasia. The immediate deformation responding to the collision is tentatively attributed to the preexisting weaknesses of the lithosphere, and therefore the deformation of the northeastern Tibetan Plateau should be regarded as a boundary-condition-dependent process.

关键词： apatite fission track Qaidam Shan Luliang Shan North Qaidam thrust belt Tibetan plateau

Deformation geometry and timing of the Wupoer thrust belt in the NE Pamir and its tectonic implications

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Frontiers of Earth Science 2016年第4期10卷 751-760页

作者： Xiaogan CHENG Hanlin CHEN xiubin lin Shufeng YANG Shenqiang CHEN Fenfen ZHANG Kang LI Zelin LIU School of Earth Sciences Zhejiang University Hangzhou 310027 China Research Center for Structures in Oil- and Gas-Bearing Basins Ministry of Education Hangzhou 310027 China Department of Exploration Geophysics College of Geophysics and Information Engineering China University of Petroleurn-Beijing Beijing 102249 China

The Pamir region, located to the northwest of the Tibetan Plateau, provides important information that can aid the understanding of the plateau＇s tectonic evolution. Here we present new findings on the deforma- tion geometry and timing of the Wupoer thrust belt at the northeastem margin of Pamir. Field investigations and interpretations of seismic profiles indicate that the eastern portion of the Wupoer thrust belt is dominated by an underlying foreland basin and an overlying piggy-back basin. A regional unconformity occurs between the Pliocene （N2） and the underlying Miocene （NI） or Paleogene （Pg） strata associated with two other local unconformities between Lower Pleistocene （Q1） and N2 and between Middle Pleistocene （Q2-4） and Q1 strata. Results of structural restorations suggest that compres- sional deformation was initiated during the latest Miocene to earliest Pliocene, contributing a total shortening magnitude of 48.6 km with a total shortening rate of 48.12%, most of which occurred in the period from the latest Miocene to earliest Pliocene. These results, com- bined with previous studies on the Kongur and Tarshkor- gan extensional system, suggest an interesting picture of strong piedmont compressional thrusting activity concur- rent with interorogen extensional rifting. Combining these results with previously published work on the lithospheric architecture of the Pamir, we propose that gravitational collapse drove the formation of simultaneous extensional and compressional structures with a weak, ductile middle crustal layer acting as a decollement along which both the extensional and compressional faults merged.

关键词： Pamir Kongur Wupoer gravitational collapse fold-and-thrust belt

Deformation features and tectonic transfer of the Gumubiezi Fault in the northwestern margin of Tarim Basin, NW China

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Petroleum Exploration and Development 2020年第4期47卷 753-761页

作者： PARIDIGULI Busuke XIE Huiwen CHENG Xiaogan WU Chao ZHANG Yuqing XU Zhenping lin xiubin CHEN Hanlin School of Earth Sciences Zhejiang UniversityHangzhou 310012China Research Center for Structures in Oil and Gas Bearing Basins Ministry of EducationHangzhou 310012China Exploration and Development Research Institute of PetroChina Tarim Oilfield Company Korla 841000China

Through field geologic survey,fine interpretation of seismic reflection data and analysis of well drilling data,the differential deformation,tectonic transfer and controlling factors of the differential deformation of the Gumubiezi Fault(GF)from east to west have been studied *** study shows that GF started to move southward as a compressive decollement along the Miocene gypsum-bearing mudstone layer in the Jidike Formation at the Early Quaternary and thrust out of the ground surface at the northern margin of the Wensu Uplift,and the Gumubiezi anticline formed on the hanging wall of the *** displacement of the GF decreases gradually from 1.21 km in the east AA′transect to 0.39 km in the west CC′transect,and completely disappears in the west of the Gumubiezi *** part of the displacement of the GF is converted into the forward thrust,and another part is absorbed by Gumubiezi *** formation of the GF is related to the gypsum-bearing mudstone layer in the Jidike Formation and barrier of the Wensu *** differential deformation of the GF from east to west is controlled by the development difference of gypsum-bearing mudstone layer in the Jidike *** the east part,gypsum-bearing mudstone layer in the Jidike Formation is thicker,the deformation of the duplex structure in the north of the profile transferred to the basin along gypsum-bearing mudstone layer;to the west of the Gumubiezi structural belt(GSB),the gypsum-bearing mudstone layer in Jidike Formation decreases in thickness,and the transfer quantity of deformation of the duplex structure along the gypsum-bearing mudstone layer to the basin gradually *** contrast,on the west DD′profile,the gypsum-bearing mudstone is not developed,the deformation of the deep duplex structure cannot be transferred along the Jidike Formation into the basin,the deep thrust fault broke to the surface and the GF disappeared *** displacement of the GF to the west eventually

关键词： Tarim Basin Wushi Sag Gumubiezi Fault deformation feature tectonic transfer deformation mechanism

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Major transgression during Late Cretaceous constrained by basin sediments in northern Africa： implication for global rise in sea level

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Frontiers of Structural and Civil Engineering 2017年第4期11卷 740-750页

作者： Kaixuan AN Hanlin CHEN xiubin lin Fang WANG Shufeng YANG Zhixin WEN Zhaoming WANG Guangya ZHANG Xiaoguang TONG School of Earth Sciences Zhejiang University Hangzhou 310027 China Research Center for Structures in Oil- and Gas-Bearing Basins Ministry of Education Hangzhou 310027 China Research Institute of Petroleum Exploration and Development PetroChina Co. Ltd Beijing 100083 China China National Oil and Gas Exploration and Development Corporation Beijing 100083 China

The global rise in sea level during the Late Cretaceous has been an issue under discussion by the international geological community. Despite the signifi- cance, its impact on the deposition of continental basins is not well known. This paper presents the systematic review on stratigraphy and sedimentary facies compiled from 22 continental basins in northern Africa. The results indicate that the region was dominated by sediments of continental facies during Early Cretaceous, which were replaced by deposits of marine facies in Late Cretaceous. The spatio- temporal distribution of sedimentary facies suggests marine facies deposition reached as far south as Taou- deni-Iullemmeden-Chad-A1 Kufra-Upper Egypt basins during Turonian to Campanian. These results indicate that northern Africa underwent significant transgression during Late Cretaceous reaching its peak during Turonian to Coniacian. This significant transgression has been attributed to the global high sea-level during this time. Previous studies show that global rise in sea level in Late Cretaceous may have been driven by an increase in the volume of ocean water （attributed to high C02 concentra- tion and subsequently warm climate） and a decrease in the volume of the ocean basin （attributed to rapid production of oceanic crust and seamounts）. Tectonic mechanism of rapid production of oceanic crust and seamounts could play a fimdamental role in driving the global rise in sea level and subsequent transgression in northern Africa during Late Cretaceous.

关键词： global sea-level changes Late Cretaceous,transgression sedimentary facies northern Africa

Establishing the present-day differential climate of Qaidam Basin since ～9 Ma driven by the uplift of Qilian Shan

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Establishing the present-day differential climate of Qaidam ...