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作 者:刘殿升
机构地区:[1]中国石油天然气总公司勘探局
出 处:《地质论评》1996年第S1期194-198,共5页Geological Review
摘 要:笔者在前人工作的基础上进行了大量的野外和室内研究工作,结合区内断裂带的分布特征、生物古地理、层序地层学及区域地质构造背景,以较为详实的资料论证了金平地区在泥盆纪时期可能为一游离于扬子地台与南方古大陆之间的一小地体,为古特提斯造山带及南北古大陆分界线的进一步研究奠定了基础。Based on the work of predecessors,large amounts of field work and indoor research were done by the author.Besides,he also studied the distribution features of the fault zone,biogeography, sequence stratigraphy and regional tectonic setting of the area.On that basis he demonstrates that the Jinping area might be a separate small terrane between the Yangtze platform and the southern paleocontinent in the Devonian,thus providing a foundation for a further study of the Paleo-Tethys orogenic belt and the boundary between the southern and northern paleocontinents.
分 类 号:P531[天文地球—古生物学与地层学]
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