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195篇 您的检索式:作者名="Sengor"
    题名 作者 年代 出处 被引量
1大别山东段高压变质岩中的金刚石显示文摘近年报道在某些超基性岩和苦橄岩中发现过金刚石。Sobolev报道了苏联北哈萨克斯坦的高压变质带中有金刚石产出,并认为是苏联西部地区(Pridneprove)第三系中金刚石砂矿的原生矿。本文报道的大别山高压变质岩中金刚石与北哈萨克斯坦变质岩中者有若干相似之处,是这类金刚石产出在世界范围内的第二例,在国内为首例。徐树桐 苏文 刘贻灿 江来利 季寿元 A. I. Okay A.M.C. Sengor 1991科学通报1991,36,17:22
2板块构造学与造山运动:特提斯例析梗概显示文摘1 引言本文是作者的题为“二十五年来的板块构造学和造山运动研究:特提斯例析”长文的极简要梗概,原文发表于《地球科学论评》(1990,Vol.271 p.1—201,下文引用以“Sengor1990a”表示),笔者在撰写梗概过程中并未试图对原文作系统修改以使之反映最新的认识,但确实增加了一些内容,并对原文的一些错误进行了修正。为使读者了解所新增的内容,文中用方括弧来表示之;所有的修正均用楷体字表示;A. M. Celal Sengor 周祖翼 丁晓 1992海洋地质译丛1992,,1:2
3造山过程中的走向滑移断层作用:特提斯地区的意义与实例显示文摘平行于造山带走向的走滑断层作用的存在及其意义在20世纪早期就已受到关注,而且板块构造为其定位提供了合理的解释。除此以外,还发展了以剖面综合为主的早期造山带板块构造模式,及其工作方法,以制作穿越整个造山带的平衡剖面,并推测深部构造。近年来,关于沿造山带的侧向运动的认识又趋普遍,这主要是由对于沿北美科迪勒拉有大量地壳断块(称为地体)的径向运动的认识引起的。Sengor A.M.C Yilmaz Y 刘俊来 1991世界地质1991,10,1:2
4Comparative orotomy of the Archean Superior and Phanerozoic Altaid orogenic systems显示文摘We compare and contrast the materials and mechanisms of continental crustal growth in the largest preserved regions of Phanerozoic and Archean juvenile additions to the crust,to test for similarities or differences in the formation of continents through time.We accomplish this through a comparison of map patterns,lithological contents,and structural and metamorphic evolution of the Phanerozoic Altaid orogenic system of Asia,with the Archean Superior Province of the North American Craton,using a method termed comparative orotomy.Both orogenic systems consist of collages of curvilinear belts of eroded arcs,some older continental slivers,and vast tracts of former subduction/accretionary complexes.These contain numerous shreds of portions of the ophiolite suite,slivers of island and continental arcs,and accreted oceanic plateau,all intruded by multiple magmatic suites during or between multiple deformation events,then sliced by large transcurrent fault systems and bent into large oroclinal structures.We make this comparison because the Superior Province is a typical Archean craton that was later,in the P aleoproterozoic,incorporated into the larger North American Craton,and has occupied a central position in several super continents(e.g.Kenorland and Nuna,which then formed the core of Columbia,Rodinia,Laurentia and Pangea)during its longevity.Since it is the largest single fragment of Archean continental cratonic lithosphere preserved on Earth,the Superior Province is widely regarded as a testing ground for how Earth’s continental crust was formed.Likewise,the Altaids encompass the largest region of crustal growth for the Phanerozoic.Our comparison with the Altaids is needed,as in recent years many myths about how the planet may have responded to higher heat production and flow in the Archean have emerged,because of trends in the science where regional geology is ignored in favor of numerical models,isotopic proxies for assumed models of chemical behavior for crust-forming or tectonic processes,or comparisons with other-worldly bodies that bear little resemblance to our hydrous Earth.Thus,we return to the geological record,and here describe the map patterns,lithological associations,structural patterns and evolution of both the Altaids and Superior Province,showing how comparative tectonics,orotomy,is useful in the absence of meaningful paleomagnetic or biostratigraphic data.We pay particular attention to the style of preservation of disaggregated members of the ophiolite suite(ophirags)and their relationships with other tectonic units,and to the widespread but largely overlooked role of late-stage major transcurrent motions and structural slicing of both Archean and Phanerozoic orogenic systems in defining the present-day architecture of both orogenic systems.Timothy M.Kusky A.M.Celal Sengor 2023National Science Review2023,10,2:2
5Relative timing of rifting and volcanism on Earth and its tectonic implications显示文摘Sengor A M C Burke K 1978Geophysical Research Letters1978,5,:1
6Plate tectonics and orogenic research after 25years: a Tethyan perspective 显示文摘Sengor A M C 1990Earth Sicence Reviews1990,27,12:1
7Coesite from the Dabie Shan eelogites, central China显示文摘Okay A I Xu S T Sengor A M 1989European Journal of Mineralogy1989,1,:1
8On a Rail Transportation Model with Scheduled Services 显示文摘Ozekici S Sengor S 1994Transportation Science1994,28,3:1
9Coesite from the Dabie Shan eclogites, central China显示文摘Okay Al Xu S T Sengor AMC 1989EurJ Mineral1989,3,:1
10Coesite from the Dabie Shan eclogites,central China显示文摘OKAY A XU S SENGOR A M 1989Eur J Mineral1989,1,:1
11Relative timing of rifting and volcanism on Earth and its tectonic implications显示文摘Sengor A M C Burke K 1978Geophys Res Lett1978,5,:1
12Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia 显示文摘Sengor A M C Natalin B A Burtman V S 1993Nature1993,364,:1
13Evolution of the Altaid tectonic collage and Paleozoic crustal growth in Eurasis显示文摘Sengor A M C Natalin B A Burtman V S 1993Nature1993,364,:1
14Evidence for intracontinental thrustrelated exhumation of the ultra-high-pressure rocks in China显示文摘Okay A I Sengor A M C 1992Geology1992,20,5:1
15The Cimmeride organic system and the tec- tonics of Eurasia显示文摘Sengor A M C 1984The Geological Society Special Paper1984,195,:1
16Evolution of the Altaid tectonic collage and Palaeozoic crustal growth in Eurasia显示文摘Sengor A M C Natal'in B A Burtman V S 1993Nature1993,364,:1
17The role of accretionary wedges in the growth of continents: Asiatic examples from Argand to Plate tectonics显示文摘Sengor A W C Okurogullari A H 1991Eclogae Geol Heir1991,84,3:1
18Evidence for intra-continental thrust related exhumation of the ultrahigh-pressure metamorphic rocks in China 显示文摘Okay A I Sengor A M C 1992Geology1992,20,:1
19JUNGGAR, Turfan and ala-kol basins as late permian to early triassic extensional structuresin a sinistral shear zone in the altaid orogenic collage, central-asia显示文摘Allen M B Sengor A Natalin B A 1995Journal of the geological society1995,152,2:1
20Tectonics of South China: Key to understanding West Pacific geology 显示文摘Hsu K J Li Jiliang Chen Haihong Wang Qingchen Sun Shu Sengor A M C 1990Tectonophysics1990,183,14:1
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