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CARBONATITES FROM THE EASTERN HIMALAYAN SYNTAXIS: PETROLOGY AND TECTONIC IMPLICATIONS

地学前缘 2000年第S1期7卷 10-11页

作者： Liu Yan 1, Zhong Dalai 2. Ji Jianqing 3(1 institute of Geology, chinese {2. of Geological sciences, beijing 100037, china 2.institute of Geology & Geophysics, chinese academy of sciences, beijing 10002., china 3 Department of Geology, Pek

Most carbonatites occur in relatively stable, intra\|plate areas but some are found to occur in near to plate margins and may be linked with plate separation (Woolley, 1989). Although many carbonatites have been discovered to occur in the orogenic belts in recent years, most of these rocks are related to post\|orogenic magmatism, that is, the rocks occur in the specially extensional setting. Therefore it is unusual that such magmatic rocks occur in the typical convergent environment. Here we report carbonatites and associated ultramafic and mafic rocks in the core of the eastern Himalayan syntaxis. The eastern Himalayan syntaxis consists of three tectonic units: the Gangdise, the Yarlung Zangbo, and the Himalayan units, each of which is bounded by faults (Liu & Zhong, 1997). The Himalayan unit, the northernmost exposed part of the Indian plate, is divided into two complexes, the amphibolite facies complex in the south and the granulite facies complex in the north. The granulite facies complex in the Himalayan unit have been argued to experience high\|pressure metamorphism and represent materials buried to upper\|mantle depths (Liu & Zhong, 1997). The carbonatites and associated ultramafic and mafic rocks only occur in the granulite facies rocks and are divided into two belts: northern and southern *** northern belt extends at least 30km, and is about 2.km in width. The southern belt extends several kilometers, and is 3km or so in width. Each belt consists mainly of differently compositional dykes, extending parallel to gneissosity of granulite facies gneiss. Carbonatitic agglomerates are observed in the northern belt. From the center of carbonatite dykes to country rocks, five types of rock are observed: the center parts of carbonatites, the rim parts of carbonatites, ultramafic and mafic rocks, altered rocks and country rocks. The gneissosity of country rock was deformed by intrusion of dykes.

关键词： Eastern Himalayan Syntaxis carbonatites ultramafic rocks carbonatitie magmatism convergent environment

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Grain Boundary Conductivities of Peridotite at High Temperature and High Pressure

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地学前缘 2009年第S1期16卷 218-219页

作者： Lidong Dai~1,Heping Li~1,Haiying Hu~(1,2.,Shuangming Shan~1 1.laboratory for Study of the Earth’s Interior and Geofluids,institute of Geochemistry,{2.,Guiyang 550002.china. 2.Graduate School of the {2.,beijing 100080,china

The grain boundary conductivities of dry synthetic peridotite are conducted by virtue of YJ-3000t multi-anvil press and Solartron-12.0 Impedance /Gain-phase Analyzer at conditions of 4.0 GPa, 1373 K and frequency rang... 详细信息

关键词： peridotite electrical conductivity oxygen fugacity

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GRANITOIDS AND TETONIC EVOLUTION OF THE WEST KUNLUN OROGENIC BELT

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地学前缘 2000年第S1期7卷 228-229页

作者： Wang Yuanlong 1,Bi Hua 2. Wang Zhonggang 2. Zhu Xiaoqing 2.(1.institute of Geology And Geophysics, {2. academy of Science, beijing 10002.,china 2.institute of Geochemistry, {2. academy of Science, Guiyang 550002.china)

The West Kunlun orogenic belt, one of the least studied areas in china, is located at the junction between the Qinghai—Tibetan Plateau and Tarim Basin and has undergone intense tectonic action and frequent *** West Kunlun orogenic belt can be divided into five tectonic\|magmatic evolution stages according to the character of the igneous rocks, metamorphic rocks, sedimentation mode, tectonic phases and isotopic ages(Fig 1).Active stages have dominated with only short intervening stable stages. This kind of evolution is not simply repeated but that a later stage is elevation and development of its former ***\|time distribution of granitoids varies with each different tectonic\| magmatic stage as well as within different periods of the same tectonic\| magmatism stage. Take time into condition , It is an important turning movement of tectonics\|magmatism evolution during the Indo\|Sinian movement, as space the middle fault (Jiang Chunfa 1982. of the West Kunlun orogenic belt is a significant border o f tectonics\|magmatism evolution. Granitoids formed before Indo\|Sinian movement are mainly distributed to the north of the middle fault of West Kunlun. These granitoids are mostly granites of early and middle Proterozoic, Caledonian and Hercynian ages. A unique control on the granitoid evolution is that they become younger from NE to SW, crossing the regional structure line. Granitoids formed after Indo\|Sinian movement are mainly distributed to the south of the middle fault. But distribution of granitoids of early Yanshan cycle cut across the middle fault of West Kunlun Mountain. Their age distribution shows a bidirectional control with the granitoids becoming younger across the regional structural lines from NE and SW boundary fault to the interior of the fracture belts.

关键词： the West Kunlun orogenic belt tectonic\|magmatic evolution gr anitoids

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CENOZOIC LARGE-SCALE STRIKE-SLIP FAULT IN WEST YUNNAN, china

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地学前缘 2000年第S1期7卷 268-269页

作者： Ji Jianqing 1, Zhong Dalai 2. Sang Haiqing 2. Zhang Liansheng 2.WT5,5”BX](1 Department of Geology, Peking University, beijing 100871,china 2.{2. of Geology and Geophysics, chinese academy of sciences, beijing 10002.,china)

During the collision between India and Eurasia, the continental compression and shorten is thought to be absorbed by the way of thickening of the Tibetan plateau crust and strike\|slip extrusion outwardly of blocks surrounding the Tibetan plateau. A series of models have been proposed recently, of which the most typical one is continental blocks extrusion by Tapponnier et al.. Virtually previous studies show that the Red River—Ailaoshan fault is the eastern boundary of extrusion Indochina displaced southward relative to South china about 2. Ma ago, and more, the western boundary of extrusion blocks is inferred to be Sijie fault in the eastern Burma. But the movement age of Sijie fault is around 13 Ma inferred from the age of Andeman Sea formation and different from that of the Red River—Ailaoshan fault. It is an important scientific problem where the western boundary of extrusion blocks is.

关键词： the western boundary of extrusion blocks Cenozoic dextral strike\|slip fault deformation age West Yunnan

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DEEP SEISMIC SOUNDING EVIDENCE FOR TECTONIC INTERACTION BETWEEN TARIM AND WEST KUNLUN MT

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地学前缘 2000年第S1期7卷 221-222页

作者： Li Qiusheng 1,Lu Deyuan 1,Gao Rui 1,Li Jingwei 2.Fan Jingyi 2.Zhang Zhiying 2.Liu wen 2.(1 Lithosphere Research Center, chinese {2. of Geological sciences, beijing 100037,china 2.562.institute, chinese {2. of Geological sciences, Hebei

The Tarim basin, located in the northern margin of Tibet, plays a key role in comprehending Tibetan plateau rapid uplift process. Focuses have been on the contribution of basin block to create high mountain (e.g.,Chen and Molnar,1977, Molnar et al.,1993, Ph. Matte, Tapponnier et al.,1996) since 1970. The models, which mainly depend on result of geological survey and other geophysical observation in the region excepted Deep Seismic Sounding, remained unsure because of blank(or absence ) of DSS data until our experiment was performed. How Tarim and west Kunlun to contact in depth ? What different is in crust structure between Tarim and west Kunlun Mt.? This is what we will reply to in our *** finished the program in 1997. A total of 12. set seismograms (with 3\|component sensors) and 18000kg (AT and TNT) dynamos were used for the DSS field project. 6 shot in Tarim basin and 1 shot in west Kunlun Mt. (Quanshuigou) had been shoot successfully. One shot (Pishan shot) is used as fan\|shape observation (offset is from 150km to 2.0km) in 6 shots located in Tarim basin. The survey line is along Hotan river across the Tarim basin from the north to the south. In particular, we carried 2. set seismic recorders to Kunlun Mt. to make a short line about 60 km as the southern tendency of our line. The seismic recorders were placed in an interval of 3km from one stations to the next and covered a distance of more than 300km. The stations have to be moved their location per 2.|shotting to form a meeting system or a tracing system (layout). Fig.1 showed our survey line and location of shot as well as recorder stations. Finally we gained 62. cassettes with original seismic record (include cassettes of shooting time recorder et al.). After data process total 1147 quite high\|quality three\|component digital records have been used to analyze. Here, only results of analyzing P wave data is given.

关键词： seismic evidence tectonic interaction Tarim West Kunlun Mt.

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MULTI-PERIODIC COLLISIONAL PROCESS BETWEEN INDIAN AND ASIAN CONTINENTS:A CASE OF EASTERN HIMALAYAN SYNTAXIS AND HENGDUAN MOUNTAINS

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地学前缘 2000年第S1期7卷 47-48页

作者： Zhong Dalai 1, Ding Lin 1, Zhang Jinjiang 1, Ji Jianqing 2.1 institute of Geology and Geophysics, {2., beijing 10002., china 2.Department of Geology, Peking University, beijing 100871, china)

Our study area covered the Eastern Himalayan Syntaxis (EHS) and its southern extension (Hengduan Mountain or western Sichuan and Yunnan (WSY)) which is located at the orthogonal and oblique collisional front between Indian and Asian continents during *** on geometric and kinematic mapping of the major boundary or regional faults (Dongjug—Mainling(1), Anigiao(2. and Jali(3), Guyu(4) faults in EHS, Ailaoshan—Red River(5), Lancangjiang(6), Gaoligong(7), Binlangjiang(8) and Magok(9) faults in WSY) (see Fig.1), especially on abundant geochronological dating of the mylonitic rocks along these faults, and coupled with magmato\|metamorphic sequences of this region, we try to deal with the temporal and spatial relationships of collisional process to answer questions such as: (1) when did collision start ? (2. is thrusting as a initial and dominant deformation mode to absorb the crustal shortening after suturing, or earlier thrusting usually followed by large\|scale strike\|slip faults? (3) are the two structural patterns coeval at times, or do they occur alternatively during deformation history? (4) are the collisional and associate uplift processes a continuous one or periodic? Insight into such questions is crucial for better understanding of the continental deformation and testing the models available or constraining a new one.

关键词： collisional process multi\|period tectonic events Eastern Himalaya

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The Crustal Shortening and Reconstruction of the Main Terranes Through Mesozoic-Cenozoic in Qinghai-Tibet Plateau

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地学前缘 2009年第S1期16卷 270-271页

作者： Meifeng Shi~(1,2.,Yalin Li~2.Ke Cao~2.1.Chengdu institute of Geology and Mineral Resources,Chengdu 610082.china. 2.School of Earth {2. and Resources,china University of Geo{2.(beijing),beijing 100083,china

It is one of hot issues in Tibetan research that is to study the mode,process and kinetics of the crustal shortening during *** this paper, on the basis of systematic collection,analysis and research of the existing data and results from Himalayas,Lhasa and Qiangtang terranes,we conducted the balanced cross-section *** the north Qiangtang,the line-balanced cross-section

关键词： Qinghai-Tibet Plateau crustal shortening shortening value terrane

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Volcanic Facies and Their Reservoirs Characteristics in Eastern china Basins

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地学前缘 2009年第S1期16卷 152-153页

作者： Chunshuang Jin~(1,2.,Dewu Qiao~2.Wenli Pan~3 1.institute of Geology and Geophysics,{2.,beijing 10002.,china. 2.Strategic Research Center of Oil & Gas Resources,Ministry of Land & Resources,beijing 100034,china 3.Geophysical Exploration Research institute of Huabei Oilfield Company,Renqiu 062.52.china

In these years,the Upper Jurassic andesitic volcanic reservoirs in Erlian basin,the Lower Cretaceous rhyolitic volcanic reservoirs in Songliao Basin,the Cretaceous rhyolitic,and the Paleogene basaltic and trachytic volcanic reservoirs in Bohai Bay Basin,and the basaltic volcanic reservoirs in Subei basin were *** more and more volcanic oil and gas fields being discovered and developed,the volcanic rocks demonstrate a great petroleum potential in eastern basins of *** volcanic facies were identified in these basins,including volcanic conduit facies,explosive facies,effusive facies。

关键词： volcanic rocks volcanic facies reservoirs porosity types

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THE NUMERICAL SIMULATE OF THE UPLIFT PROCESS OF THE QINGHAI—TIBET PLATEAU

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地学前缘 2000年第S1期7卷 359-361页

作者： Cui Junwen 1, Shi Jinsong 2.Li Pengwu 1,Li Li 1[WT5,5”BX](1 institute of Geology, chinese {2. of Geological sciences, beijing 100372.china 2.Hoha University, Nanjing 2.0098,china)

The quantitative analysis of uplift process of the Qinghai—Tibet plateau is a key to deepen the study of uplift mechanism and dynamic model, for this, numerical simulate was done to the whole process of uplift of the Qinghai—Tibet plateau.1 Geological model According to the tectonic evolution and lithospheric structure, continental crust in the Qinghai—Tibet plateau in profile is divided into sedimentary cover, crystalline rock formation and lower crust and composed of Kunlun, Bayan Har, Qiangtang, Gangdise and Himalaya blocks on the plane. Layer or block is bounded the detachment layer or large fault. On the basis of the uplift characteristics, the calculated time limit is in the Cenozoic since 65Ma, roughly four stages, i.e., 65 to 40Ma, 40 to 2.Ma, 2. to 3Ma and 3Ma to now. Mesh profile used Yadong—Golmud Geoscience transect.

关键词： Uplift dynamic process numerical simulate shortening thickening stress strain rate of increasing temperature(RIT)

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High-Resolution Sequence Stratigraphy and Coal Accumulating Models of the Permo-Carboniferous Coal Measures in Southwestern Shanxi

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地学前缘 2009年第S1期16卷 143-144页

作者： Zhenghui Xiao~(1,2.,Longyi Shao~2.Hao Wang~2.Jing Lu~2.1.Hunan University of Science and Technology,Xiangtan 4112.1,china. 2.Department of Resources and Earth sciences,china University of Mining and Technology(beijing),beijing 100083,china

The Qinshui Basin in southeastern Shanxi Province is an important base for coalbed methane exploration and production in *** methane reservoirs in this area are the Carboniferous and Permian coals and their thickness are strongly controlled by the depositional environments and the sequence stratigraphic *** paper analyzes the high-resolution sequence stratigraphy of the Permo-Carbo-

关键词： sequence stratigraphic framework coal-accumulating model Permo-Carboniferous Qinshui Basin

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