王训练
主要从事珊瑚古生物、地层学和历史大地构造学研究。
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- 姓名:王训练
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学术头衔:
博士生导师
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学科领域:
古生物学
- 研究兴趣:主要从事珊瑚古生物、地层学和历史大地构造学研究。
王训练,男,汉族,1958年9月生,陕西武功人。1985年7月参加工作,理学博士,教授,博士生导师。1978年9月至1982年7月,在武汉地质学院地质系古生物学与地层学专业本科学习。1982年9月至1985年7月,在武汉地质学院北京研究生部古生物学与地层学专业硕士研究生学习。1985年7月至1993年10月,在中国地质大学(北京)任教。期间,1989年9月至1993年10月,在中国地质大学(北京)地质系古生物学与地层学专业博士研究生学习。其中,1990年10月至1991年9月,在东北师范大学赴日本留学生预备学校进修。1991年10月至1993年10月,在日本北海道大学地质系古生物学与地层学专业博士研究生学习。1993年10月至1995年10月,中国地质大学(北京)博士后。1995年10月至今在中国地质大学(北京)工作,2000年12月至2003年4月,任地球科学与资源学院副院长。2003年4月至2004年1月,任研究生院副院长。2004年1月至今,任地球科学与资源学院院长。2007年7月至今,任中国地质大学(北京)副校长。
主要从事珊瑚古生物、地层学和历史大地构造学研究。先后承担部级和部级以上科研项目16项。其中6项为项目负责人,3项为专题负责人。出版专著2部,文集2部,发表论文60余篇,6篇论文被SCI收录。2003年获国土资源部科学技术一等奖(排名第5),2004年获得北京市五一劳动奖章,2004年获得北京市教学成果二等奖(排名第2)。
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王训练, WANG Xunlian
SCIENCE IN CHINA (Series D) November 2002 Vol. 45 No.11,-0001,():
-1年11月30日
The steps and methods for the establishment of the global boundary stratotype section and point (GSSP) are summed up briefly as follows. (i) Select rock sequences of approximately the same age duration in a region, make a thorough study of their properties or attributes in order to establish the high-resolution stratigraphic units reflecting the natural rhythms in Earth’s history, and proceed by multidisciplinary comprehensive studies to reveal the relationship, including time-space relation and possible mutual causality, among the various stratigraphic units and the different natural rhythms established. (ii) Seek for the "natural break" that represents the "major natural changes in the historical development of the Earth" in shallow marine facies areas, which is frequently the third-order sequence boundaries. (iii) Trace from shallow marine facies areas toward the continental slope and bathyal areas to seek for a continuous depositional sequence that corresponds in time span to the "natural break" of shallow marine facies areas. (iv) Seek for a horizon within the continuous depositional sequence that approximately coincides with the maximum regressive point in the "natural break". This horizon is commonly within a lowerstand systems tract (LST) or a shelf margin systems tract (SMST) of the relevant third-order sequence. (v) Seek immediately above this horizon of maximum marine regression for an organic radiation or explosion event closely related to the natural boundary, which is generally the first flooding surface (FFS) of the relevant third-order sequence. (vi) Select within the organic event deposits closely related to the FFS the base boundary of a fossil taxon with widest geographical range as the Leading Group biozone for designation of the stratigraphic boundary. (vii) Select from among the sections with continuous depositional sequence formed under similar sedimentary palaeogeographic background (in general continental slope or bathyal environments) the section which possesses the shortest distance between the base boundary of the Leading Group biozone and the immediately underlying FFS of the relevant third-order sequence as the global stratotype section. The first appearance datum (FAD) of the Leading Group biozone species in the section may be regarded as the ideal GSSP. The steps suggested above are a supplement and improvement of the currently used procedures and methods for establishing GSSP. The GSSP established by using the steps and methods suggested here would make the stratigraphic boundaries better reflect the "major natural changes in the historical development of the Earth", more readily distinguishable and easily operable in recognition and correlation, and at the same time also make the designation of boundaries more objective.
GSSP,, the first flooding surface,, integrated stratigraphy,, chronostratigraphy,, sequence stratigraphy,, theoretical stratigraphy.,
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【期刊论文】An important reference criterion for the selection of GSSP
王训练, WANG Xunlian & SU Wenbo
Chinese Science Bulletin Vol. 45 No.5 March 2000,-0001,():
-1年11月30日
A study on the relationship between biostratigraphy and sequence stratigraphy in several designated global boundary stratotypes shows that the best way may be to take the GSSP at a point coincident with the base of the first widespread Leading Group biozone above the first flooding surface (FFS) of the relevant third-order sequence. It is suggested that the first flooding surface of the sequence should be an important reference criterion for the selection of GSSP. As the base of the first widespread Leading Group biozone chosen for the definition of GSSP could not be lower than the first flooding surface of the referred sequence, the latter surface may be an important criterion for the recognition and correlation of the chronostratigraphic boundaries.
GSSP,, first flooding surface,, sequence stratigraphy,, chronostratigraphy,, theoretical stratigraphy.,
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【期刊论文】On the tectonic position of the Baoshan region during the Late Palaeozoic
王训练, Wang Xunlian, * Kato Makotot and Wang Hongzhen*
Journal of Southemr Asim Earrk Sckwcrs. Vol. 13. Nos 3-5. pp. 171-183. 1996,-0001,():
-1年11月30日
The aim of this study is to discuss the tectonic position of Baoshan in Yunnan Province, China, during the Late Paleozoic by comparison of the sedimentary facies, fauna and palaeomagnetic data from the Baoshan region with those from the Yangtze region and southern Tibet. The sedimentary facies change suggests that in the Late Palaeozoic the Baoshan region underwent a similar geological history to southern Tibet, but different from that of the Yangtze region. The rugose corals and brachiopods as well as vertebrates of Baoshan are different from those of the Yangtze region during the Late Palaeozoic. An evident segregation seems to exist between them. The Late Paleozoic fauna of Baoshan shows certain similarities to southern Tibet. The Devonian and Late Carboniferous faunas, especially, are very similar to those in southern Tibet. This indicates that there was no evident segregation between them in the Late Palaeozoic. The palaeomagnetic data reveal that in the Late Palaeozoic the Yangtze region was close to the equator, while the Baoshan region and southern Tibet were situated in the middle latitudes. On the basis of the palaeontological, sedimentological and palaeomagnetic data, it is inferred that Baoshan and southern Tibet were situated in the same continental margin, and both regions were far from the Yangtze region during the Late Paleozoic. The Baoshan region may be considered as a massif within the Gondwana tectonic domain which includes southern Tibet, while the Yangtze region was located in another tectonic domain--the South Asian domain, with a wide ocean, the Tethys between them. Copyright 0 1996 Published by Elsevier Science Ltd.
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