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Extensional Tectonic System of Erlian Fault Basin Groupand Its Deep Background
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作者 Ren Jianye Li Sitian Faculty of Earth Resources, China University of Geosciences, Wuhan 430074 Jiao Guihao Exploration and Development Research Institute, Huabei Oil Administration Bureau, Renqiu 062552 Chen Ping Faculty of Business Administratio 《Journal of Earth Science》 SCIE CAS CSCD 1998年第3期44-49,共6页
The Erlian fault basin group, a typical Basin and Range type fault basin group, was formed during Late Jurassic to Early Cretaceous, in which there are rich coal, oil and gas resources. In the present paper the abund... The Erlian fault basin group, a typical Basin and Range type fault basin group, was formed during Late Jurassic to Early Cretaceous, in which there are rich coal, oil and gas resources. In the present paper the abundant geological and petroleum information accumulated in process of industry oil and gas exploration and development of the Erlian basin group is comprehensively analyzed, the structures related to formation of basin are systematically studied, and the complete extensional tectonic system of this basin under conditions of wide rift setting and low extensional ratio is revealed by contrasting study with Basin and Range Province of the western America. Based on the above studies and achievements of the former workers, the deep background of the basin development is treated. 展开更多
关键词 Late Mesozoic rifting extensional tectonic system deep process Erlian fault basin group.
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Reservoir Characteristics and Favorable Area Prediction of Chang-6 Reservoir in Zhouguan Area, Ordos Basin
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作者 Yuchuan Liu Mingju Tang Shengli Gao 《Journal of Geoscience and Environment Protection》 2023年第8期22-32,共21页
Based on the analysis of a large number of core samples, logging results, logging interpretation data and dynamic data in the study area, the characteristics of Chang 6 reservoir in Zhouguan area of Baihe area are stu... Based on the analysis of a large number of core samples, logging results, logging interpretation data and dynamic data in the study area, the characteristics of Chang 6 reservoir in Zhouguan area of Baihe area are studied, and the favorable reservoir areas in the study area are predicted. The results show that the lithology of Chang 6 reservoir is mainly light gray and gray fine-grained to very fine-grained feldspar lithic sandstone. The pore types are mainly residual intergranular pores and feldspar dissolved pores, including debris dissolved pores and microfractures. The porosity and permeability values are low, which belongs to low porosity-low permeability and ultra-low permeability reservoirs. According to the reservoir distribution characteristics and related data, the Chang 6 reservoir in the study area is divided into two types, mainly Class II and Class III reservoirs. The comprehensive evaluation predicts that the spatial distribution of the favorable area of Chang 6 reservoir is not uniform, but the distribution area is large, which has broad exploration and development value, and provides the necessary conditions for the distribution study of the favorable oil-bearing zone in this area and the preparation for the next exploration and development. 展开更多
关键词 extension group Baihe Oil Region Sedimentary Microfacies Basic Characteristics of Reservoir Favorable Zone
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马超营断裂以北熊耳群火山岩系是形成于弧后裂陷盆地环境的基性-酸性双峰态火山岩组合吗?——与胡德祥等同志商榷 被引量:2
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作者 郭继春 姚文平 许红忠 《地球科学(中国地质大学学报)》 EI CAS CSCD 北大核心 1992年第4期481-484,共4页
中元古界熊耳群火山岩分布于华北地台南缘。本文提出马超营断裂以北火山岩是以安山岩占主导地位的玄武岩—安山岩—英安岩—流纹岩组合,而不是胡德祥等人提出的基性—酸性双峰态组合,它们形成的构造环境为安第斯型火山弧。火山岩上部的... 中元古界熊耳群火山岩分布于华北地台南缘。本文提出马超营断裂以北火山岩是以安山岩占主导地位的玄武岩—安山岩—英安岩—流纹岩组合,而不是胡德祥等人提出的基性—酸性双峰态组合,它们形成的构造环境为安第斯型火山弧。火山岩上部的粗安岩—粗面岩组合形成的构造环境为弧内盆地。 展开更多
关键词 火山岩 熊耳群 组合 马超营 断裂
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商南地区秦岭群中的韧性伸展构造 被引量:3
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作者 裴先治 胡能高 高进龙 《地球科学与环境学报》 CAS 1993年第S1期46-53,共8页
在秦岭造山带核部秦岭群变质岩系中,发育有自NWW向SEE方向拉伸的深层次韧性伸展构造。表现为具有定的代表伸展运动方向的塑性拉伸线理、不对称顺层韧性剪切褶皱及横向置换面理等。态因后期挤压收缩作用已发生改变。伸展作用发生于加里... 在秦岭造山带核部秦岭群变质岩系中,发育有自NWW向SEE方向拉伸的深层次韧性伸展构造。表现为具有定的代表伸展运动方向的塑性拉伸线理、不对称顺层韧性剪切褶皱及横向置换面理等。态因后期挤压收缩作用已发生改变。伸展作用发生于加里东期挤压收缩、构造叠置、陆壳增厚之后,与晚加里东—早海西期大量花岗质深成岩体的上隆侵位密切相关,伸展作用方向近平行造山带走向,时代可能为早海西期。 展开更多
关键词 秦岭群 韧性伸展构造 早海西期 商南
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西秦岭造山带早白垩世大陆裂谷存在的依据——青海同仁地区麦秀山群新建的意义 被引量:10
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作者 祁生胜 邓晋福 +3 位作者 赵呈祥 胡旭丽 史连昌 陈健 《地质通报》 CAS CSCD 北大核心 2011年第11期1706-1715,共10页
青海省唯一的一套早白垩世陆相火山岩地层分布在青海省黄南州同仁县—泽库县之间的麦秀山一带,位于西秦岭地层区泽库地层分区。根据剖面研究和区域地层对比,将这套地层新命名为早白垩世麦秀山群(K1M),下部的紫红—灰紫色中基性火山岩夹... 青海省唯一的一套早白垩世陆相火山岩地层分布在青海省黄南州同仁县—泽库县之间的麦秀山一带,位于西秦岭地层区泽库地层分区。根据剖面研究和区域地层对比,将这套地层新命名为早白垩世麦秀山群(K1M),下部的紫红—灰紫色中基性火山岩夹砂砾岩新建为多禾茂组(K1d),为一套典型的陆相裂隙式喷发的碱性玄武岩+陆相红层沉积建造,上部的紫红色砂砾岩组合延用万秀组(K1w),为一套冲积扇相陆相红层的类磨拉石建造,二者之间为明显的整合接触关系。根据麦秀山群与上下地层之间的角度不整合接触关系,以及多禾茂组火山岩中的同位素年龄和万秀组的昆虫、叶肢介、植物化石,可确定麦秀山群的形成时代为早白垩世。麦秀山群沿近南北向张裂带分布,是在早白垩世陆内环境下产生并在陆内环境下消亡的陆内裂谷相沉积,它的形成标志着西秦岭地区在早白垩世进入区域性伸展阶段。 展开更多
关键词 西秦岭造山带 早白垩世 麦秀山群陆内裂谷伸展环境
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辽宁海城地区辽河群底部大型韧性滑脱带的构造演化 被引量:6
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作者 刘永江 李三忠 白立新 《长春地质学院学报》 CSCD 1996年第2期166-171,共6页
通过对辽宁海城地区赵家堡子-马风-什司县一带早元古宙辽河群底部地层和变质深成侵入体的详细构造研究,确认了辽河群底部与太古宙之间大型韧性滑脱带的存在。卷入滑脱带的地质体有辽河群底部浪子山岩组和早元古宙变质深成侵入体。滑... 通过对辽宁海城地区赵家堡子-马风-什司县一带早元古宙辽河群底部地层和变质深成侵入体的详细构造研究,确认了辽河群底部与太古宙之间大型韧性滑脱带的存在。卷入滑脱带的地质体有辽河群底部浪子山岩组和早元古宙变质深成侵入体。滑脱带的构造演化可划分为:①吕梁运动早期沿太古宙与早元古宙接触带部位发生大规模拉伸顺层滑脱变形作用;②拉伸滑脱变形中晚期早元古宙深成侵入体沿滑脱带顺层同构造就位;③吕梁运动晚期滑脱带的收缩变形作用三大阶段。 展开更多
关键词 辽河群 变形作用 构造演化 地层 早元古宙
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二连断陷盆地群伸展构造系统及其发育的深部背景 被引量:54
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作者 任建业 李思田 焦贵浩 《地球科学(中国地质大学学报)》 EI CAS CSCD 北大核心 1998年第6期567-572,共6页
二连盆地形成于侏罗纪到早白垩世期间,是东北亚断陷盆地系内的一个典型的盆岭式断陷盆地群,其内蕴藏丰富的煤和油气资源.综合分析了二连盆地油气勘探中积累的地质资料,系统地研究了与盆地形成有关的构造,并与北美西部盆岭省进行了... 二连盆地形成于侏罗纪到早白垩世期间,是东北亚断陷盆地系内的一个典型的盆岭式断陷盆地群,其内蕴藏丰富的煤和油气资源.综合分析了二连盆地油气勘探中积累的地质资料,系统地研究了与盆地形成有关的构造,并与北美西部盆岭省进行了对比,揭示了二连盆地宽裂陷作用和低拉伸率条件下的伸展构造系统.以上述研究和前人的研究成果为基础,探讨了盆地发育的深部背景. 展开更多
关键词 裂陷作用 伸展构造系统 盆地 深部背景 油气地质
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行正交矩阵的并元加性群扩大法
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作者 孙鹏勇 《辽宁工程技术大学学报(自然科学版)》 CAS 2000年第3期298-301,共4页
利用m-并元加性群(m是素数),本文提出了行正交矩阵的一种扩大法.利用这种扩大法可以得到一系列延续矩阵.
关键词 矩阵扩大法 行正交矩阵 并元加性群 延续矩阵
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泌阳凹陷复杂断鼻构造样式解析 被引量:3
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作者 朱军 李连生 +3 位作者 李辉 孙峥嵘 季玉瑶 苏桂芝 《河南石油》 2004年第2期5-7,共3页
泌阳凹陷在区域性引张作用下形成了典型的伸展构造样式——被不同层次断层切割成的一系列复杂断鼻、断块。通过对不同地区复杂断鼻、断块构造特征的研究,总结出地堑和阶梯状两种断块群模式类型,并对其控油机制进行分析,指出继承性的鼻... 泌阳凹陷在区域性引张作用下形成了典型的伸展构造样式——被不同层次断层切割成的一系列复杂断鼻、断块。通过对不同地区复杂断鼻、断块构造特征的研究,总结出地堑和阶梯状两种断块群模式类型,并对其控油机制进行分析,指出继承性的鼻状构造不仅控制了泌阳凹陷油气聚集的方向,也控制着各区的油气富集程度;断层是复杂断鼻构造油气成藏的主要因素,既可成为油气运移的通道,又可阻挡油气的运移而聚集成藏。因此泌阳凹陷复杂断鼻构造具备形成大面积油气富集区的地质条件。 展开更多
关键词 泌阳凹陷 伸展构造 断鼻断块群 地堑断块 阶梯断块
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山西吕梁地区汉高山群火山岩成因及其形成环境 被引量:2
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作者 雷天 张成立 +2 位作者 白海峰 刘欣雨 杨欢 《地质学报》 EI CAS CSCD 北大核心 2022年第2期465-481,共17页
吕梁地区汉高山群火山沉积岩是华北克拉通中部带中部中元古代初期火山-沉积记录,其成因及形成环境研究对认识华北克拉通结晶基底固结后地质演化有重要意义。该群火山岩为拉斑玄武系列安山岩,SiO_(2)(54.68%~56.19%)略低,有较高的MgO(4.9... 吕梁地区汉高山群火山沉积岩是华北克拉通中部带中部中元古代初期火山-沉积记录,其成因及形成环境研究对认识华北克拉通结晶基底固结后地质演化有重要意义。该群火山岩为拉斑玄武系列安山岩,SiO_(2)(54.68%~56.19%)略低,有较高的MgO(4.97%~6.16%,Mg;=49.4~53.8)及Cr(165×10^(-6)~174×10^(-6))和Ni(31.1×10^(-6)~34.2×10^(-6))含量,高TiO_(2)(1.34%~1.40%),TFeO/MgO=1.70~2.03,富集LREEs和Ba、U、K等LILEs,亏损Nb、Ta、Ti等HFSEs,与弧岩浆地球化学特征类似。它们的ε;(t)偏负且变化小(-4.48~-4.31),T;=2509~2520 Ma,其高的Ba/Th和低的(La/Sm);说明它们源自受板片俯冲流体改造的岩石圈地幔,地幔改造为新太古代大洋板片消减所致。结合邻区小两岭组火山岩和华北克拉通南部熊耳群火山岩也显示弧岩浆地球化学特征,且Sr-Nd同位素组成揭示源自新太古代板片俯冲改造的岩石圈地幔,与同期基性岩墙群一道代表板内伸展环境岩浆活动的产物,而非为弧岩浆活动的记录,代表了华北克拉通中元古代初期转入大陆伸展拉张环境,首套火山沉积建造,是全球Columbian超大陆裂解初期在华北地块的物质记录。 展开更多
关键词 汉高山群 安山岩 伸展背景 大陆岩石圈地幔 吕梁地区 华北克拉通
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Conjugacy Classes and Characters for Extensions of Finite Groups
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作者 Xiang TANG Hsian-Hua TSENG 《Chinese Annals of Mathematics,Series B》 SCIE CSCD 2014年第5期743-750,共8页
Let H be an extension of a finite group Q by a finite group G. Inspired by the results of duality theorems for etale gerbes on orbifolds, the authors describe the number of conjugacy classes of H that map to the same ... Let H be an extension of a finite group Q by a finite group G. Inspired by the results of duality theorems for etale gerbes on orbifolds, the authors describe the number of conjugacy classes of H that map to the same conjugacy class of Q. Furthermore, a generalization of the orthogonality relation between characters of G is proved. 展开更多
关键词 group extensions Conjugacy classes Orthogonality of characters2000 MR Subject Classification 20E22 20C05
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耀岭河群地球化学特征及其意义 被引量:4
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作者 王寿琼 《湖北地质》 1995年第2期72-83,共12页
笔者通过地球化学经典国解和参数研究了耀岭河群基性火山岩的地球化学特征、构造环境、物源及岩石成因。研究表明,该基性火山岩为稳定-半稳定环境下的张性岩套,喷发物源可能是经原始地幔交代的富集型洋中脊玄武岩,具地慢热栓的特点... 笔者通过地球化学经典国解和参数研究了耀岭河群基性火山岩的地球化学特征、构造环境、物源及岩石成因。研究表明,该基性火山岩为稳定-半稳定环境下的张性岩套,喷发物源可能是经原始地幔交代的富集型洋中脊玄武岩,具地慢热栓的特点,显示古板块分别向西南和北东方向扩张。其构造环境属继承早期陆内裂谷发展而成边缘海盆地的大陆边缘裂谷带。 展开更多
关键词 耀岭河群 张性岩套 地幔热栓 裂谷
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Agricultural extension approach:evidence from an Integrated Soil Fertility Management Project in Ethiopia
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作者 Gerba LETA Steffen SCHULZ Girum GETACHEWALEMU 《Frontiers of Agricultural Science and Engineering》 2020年第4期427-439,共13页
Agricultural extension is an approach to rural development and agricultural transformation in which training,demonstration and technology transfer are key to reducing rural poverty,ensuring food security,and sustainab... Agricultural extension is an approach to rural development and agricultural transformation in which training,demonstration and technology transfer are key to reducing rural poverty,ensuring food security,and sustainably managing natural resources.During recent decades,different extension approaches have been tested and validated by the Ethiopian government and nongovernmental organizations to stimulate participation in the agricultural extension system(AES).The most recent was a German-funded project entitled“Integrated Soil Fertility Management Project”(ISFM+),which employed a novel approach to piloting and upscaling proven technology and best practice.The purpose of this study was to analyze and document the modalities of ISFM+and illustrate its effects on technology uptake and dissemination.The study used a mixed methods approach to collect data.ATLAS.ti and SPSS were used for data management and analysis.Farmer Research and Extension Groups and Farmer Field Schools were found to be central to the participation process.Also,the ISFM+was found to aid technology transfer and helped to increase grain and residue yields as well as farmer livelihoods.Based on these empirical findings,it is argued that the ISFM+approach and technology should be integrated and institutionalized in the mainstream AES in order to promote their extensive application. 展开更多
关键词 Ethiopia Farmer Field School Farmer Research and extension group GOVERNANCE INSTITUTIONALIZATION ISFM+ambassador PARTICIPATION
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Lifting of Outer Actions of Groups
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作者 Fang ZHOU He Guo LIU 《Acta Mathematica Sinica,English Series》 SCIE CSCD 2010年第9期1693-1700,共8页
Let G and N be arbitrary groups. In this paper, we construct an associated group extension εx of N/Z(N) by G for any group homomorphism X : G → Out N, and prove that X can be lifted to a group action, that is, a ... Let G and N be arbitrary groups. In this paper, we construct an associated group extension εx of N/Z(N) by G for any group homomorphism X : G → Out N, and prove that X can be lifted to a group action, that is, a group homomorphism from G to Aut N, if and only if the extension εx splits. Furthermore we obtain an explicit description for all such lifting homomorphisms and the number of its conjugacy classes, and give an application of the lifting technique of outer actions to the theory of group extensions. 展开更多
关键词 Outer action group extension LIFTING
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On K_2-group of a Formal Matrix Ring
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作者 Zi Qiang FAN Zhi Xiang YIN 《Acta Mathematica Sinica,English Series》 SCIE CSCD 2012年第9期1897-1906,共10页
Let S be a formal matrix ring, T the subring consisting of all diagonal elements, I the set consisting of all off-diagonal elements. Then I is a split radical ideal under certain conditions. In this paper, we show tha... Let S be a formal matrix ring, T the subring consisting of all diagonal elements, I the set consisting of all off-diagonal elements. Then I is a split radical ideal under certain conditions. In this paper, we show that K2(S)≈ K2(T) G K2(S, I), and a presentation of K2(S, I) is given. 展开更多
关键词 K2 group relative K2 group extension of groups
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Structural architecture of Neoproterozoic rifting depression groups in the Tarim Basin and their formation dynamics 被引量:3
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作者 Bizhu HE Cunli JIAO +10 位作者 Taizhu HUANG Xingui ZHOU Zhihui CAI Zicheng CAO Zhongzheng JIANG Junwen CUI Zhuoyin YU Weiwei CHEN Ruohan LIU Xiaorui YUN Guangming HAO 《Science China Earth Sciences》 SCIE EI CAS CSCD 2019年第3期529-549,共21页
The Tarim Basin is the largest, oil-bearing, superimposed basin in the northwest of China. The evolution and tectonic properties of the initial Tarim Basin have been hotly disputed and remain enigmatic. The Neoprotero... The Tarim Basin is the largest, oil-bearing, superimposed basin in the northwest of China. The evolution and tectonic properties of the initial Tarim Basin have been hotly disputed and remain enigmatic. The Neoproterozoic basin is covered by a vast desert and a huge-thickness of sedimentary strata, has experienced multiple tectonic movements, had a low signal to noise ratios(SNRs) of deep seismic reflection data, all of which have posed critical obstacles to research. We analysed four field outcrops, 18 wells distributed throughout the basin, 27 reprocessed seismic reflection profiles with higher SNRs across the basin and many ancillary local 2D and 3D profiles and aeromagnetic data. We found about 20 normal fault-controlled rifting depressions of the Cryogenian and Ediacaran scattered throughout the basin, which developed on the Precambrian metamorphic and crystalline basement. The structural framework is clearly different from that of the overlying Phanerozoic. The rifting depressions consist of mainly half grabens, symmetrical troughs and horst-grabens. From the northeast to southwest of the basin,they are divided into three rifting depression groups with the WNW, ENE, and NW-trends that are mainly controlled by normal faults. The maximum thicknesses of the strata are up to 4100 m. From the Cryogenian to Ediacaran, most of the main inherited faults to active and eventually ceased at the end of the Ediacaran or Early Cambrian, while subsidence centres appeared and migrated eastward along the faults. They revealed that the different parts of the Tarim continental block were in NNE-SSWoriented and NNW-SSE-oriented extensional paleo-stress fields(relative to the present) during the Neoproterozoic, and were accompanied by clockwise shearing. According to the analysis of the activities of syn-sedimentary faults, filling sediments,magmatic events, and coordination with aeromagnetic anomalies, the tectonic properties of the fault depressions are different and are primarily continental rifts or intra-continental fault-controlled basins. The rifting phases mainly occurred from 0.8–0.61 Ga.The formation of the rifting depression was associated with the initial opening of the South Altun-West Kunlun Ocean and the South Tianshan Ocean, which were located at the northern and southern margins of the Tarim Block, respectively, in response to the break-up of the Supercontinent Rodinia and the initial opening of the Proto-Tethys Ocean. 展开更多
关键词 RIFTING DEPRESSION groups Normal faults extensional and clockwise shearing CRYOGENIAN and EDIACARAN Continental rift and intra-continental fault-controlled BASIN Tarim BASIN
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Morita Equivalences Induced by Two-Sided Group Relative Hopf-Module
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作者 Qiao Ling GUO Qi Hui LI Rui Fang HU 《Journal of Mathematical Research and Exposition》 CSCD 2011年第5期819-828,共10页
Let H be a Hopf π-coalgebra over a commutative ring k with bijective antipode S, and A and B right π-H-comodulelike algebras. We show that the pair of adjoint functors (F3 = A Bop A□ HBop -,G3 = (-)coH) betwee... Let H be a Hopf π-coalgebra over a commutative ring k with bijective antipode S, and A and B right π-H-comodulelike algebras. We show that the pair of adjoint functors (F3 = A Bop A□ HBop -,G3 = (-)coH) between the categories A□HBopM and AMπB-H is a pair of inverse equivalences, when A is a faithfully flat π-H-Galois extension. Furthermore, the categories Moritaπ-H(A,B) and Morita □π-H(AcoH,BcoH) are equivalent, if A and B are faithfully flat π-H-Galois extensions. 展开更多
关键词 Hopf group Galois extension Morita equivalence group relative Hopf-module.
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