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NO.1.I’reface………’··’…………’…………‘…··‘…………………………………………Zhal Yu。lleng(l)bteletal btructures and Classlflcatlon of the Order Cystlpbylllda(Rugosa)…………………………………… Wang I4ongzhen,He Yuan-clang and Chen Jlanqlang(3)I。oramlnlfera Blostratl匡raphy and Paleogeography of the T。rtlary In Tibet Was X laoqiao(15)Trace Fossils In Ngar。l{eglon,Xlzang(tibet)and their Sedimentary Environments………………………………………··‘……………………………h…  相似文献   

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《现代地质》1988,2(4):526
N口.D.Palaeozolc >mall,r Foramlnlfera Fauna、on the East Part of 八Orth China Platform… ··’…·’··’”……··””·’”……’……·”…··”’…………………………··Zheng hong(19)Tge Character5of Sllurlan Rugose Corals and the Discuss】on about the Age of tile Strata of Qujlnz Reg。on.Yu。nan··,,……·,··,,……,·,………,…··,··,…,…Dlnrr Chunmine(22〕sell—e口tarV rades and Te口tono—paleogeographv of the Late sin二an nengving ror回口ation In yor。bwest。rn Hubel…  相似文献   

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The Mesozoic and Cenozoic Exhumation History of Tianshan and Comparative Studies on the Junggar and Altay Mountains GUO Zhaojie, ZHANG Zhicheng, WU Chaodong, FANG Shihu and ZHANG Rui (Key Laboratory of Orogenic Belts and Crustal Evolution (Peking University), Ministry of Education, Beijing 100871) The Tianshan Mountain is a Cenozoic intracontinental orogenic belt. To constrain its deformation history during the Mesozoic and Cenozoic, we conducted integrated research on apat…  相似文献   

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