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The ICS International Chronostratigraphic Chart 被引量:27
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作者 K.M.Cohen s.c.finney +1 位作者 P.L.Gibbard J.-X.Fan 《Episodes》 2013年第3期199-204,共6页
The International Commission on Stratigraphy(ICS)has a long tradition of producing international charts that communicate higher-order divisions of geological time and actual knowledge on the absolute numerical ages of... The International Commission on Stratigraphy(ICS)has a long tradition of producing international charts that communicate higher-order divisions of geological time and actual knowledge on the absolute numerical ages of their boundaries.The primary objective of ICS is to define precisely a global standard set of timecorrelative units(Systems,Series,and Stages)for stratigraphic successions worldwide.These units are,in turn,the basis for the Periods,Epochs and Ages of the Geological Time Scale.Setting an international global standard is fundamental for expressing geological knowledge.It is also of considerable pragmatic importance as it provides the framework through which regional-scale higher-resolution divisions can be linked,equated and collated.This is a status update on the International Chronostratigraphic Chart and the ICS website www.stratigraphy.org. 展开更多
关键词 international chronostratigraphic chart timecorrelative units geological time international commission stratigraphy ics stratigraphic successions absolute numerical ages PERIODS international charts
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Ordovician of Iberia–Report on the 11^(th)International Symposium on the Ordovician System
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作者 D.L.Bruton s.c.finney I.G.Percival 《Episodes》 2011年第4期270-273,共4页
9-13 May 2011,Madrid,Spain The Iberian Peninsula is well known for its extensive outcrops of early Palaeozoic rocks and its high palaeo-latitudinal position during the Ordovician on the southern polar margin of Gondwa... 9-13 May 2011,Madrid,Spain The Iberian Peninsula is well known for its extensive outcrops of early Palaeozoic rocks and its high palaeo-latitudinal position during the Ordovician on the southern polar margin of Gondwana,had profound affects on the faunas and facies of the time.It was therefore timely that more than 120 participants from 26 countries took part in the programme consisting of three days of lectures,a mid-symposium and pre-and postsymposium field trips,described herein. 展开更多
关键词 early palaeozoic rocks palaeozoic rocks international symposium IBERIA palaeo latitudinal position faunas Gondwana ORDOVICIAN
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奥陶系上统赫南特阶全球层型剖面和点位的建立 被引量:50
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作者 陈旭 戎嘉余 +7 位作者 樊隽轩 詹仁斌 C.E.Mitchell D.A.T.Harper M.J.Melchin 彭平安 s.c.finney 汪啸风 《地层学杂志》 CSCD 北大核心 2006年第4期289-305,T0001-T0002,共19页
赫南特阶(上奥陶统)的全球界线层型剖面和点位确立在中国宜昌王家湾北剖面观音桥层底界之下0.39m处。该剖面位于中国湖北省宜昌市以北42km处的王家湾村,经纬度为30°58′56″N、111°25′10″E。赫南特阶底界的GSSP点位以笔石No... 赫南特阶(上奥陶统)的全球界线层型剖面和点位确立在中国宜昌王家湾北剖面观音桥层底界之下0.39m处。该剖面位于中国湖北省宜昌市以北42km处的王家湾村,经纬度为30°58′56″N、111°25′10″E。赫南特阶底界的GSSP点位以笔石Normalograptusextraordinarius的首次出现层位(FAD)为标志。碳同位素在此层位显示的正漂移以及N.ojsuensis的首现可作为第二标志。赫南特阶始于自Diceratograptusmirus亚带开始的全球生物大灭绝事件的主幕之后。王家湾北剖面出露完整,沉积和生物序列连续,笔石和壳相动物化石丰富并保存良好,王家湾北、王家湾南和王家湾小河边剖面都发育了合适的沉积相和生物相并具有广泛对比的潜力。该地区地质构造简单,岩石未经历较强的变质作用,且交通便利。王家湾小河边剖面尤其适合进行化学地层学研究和同位素年龄的测定。建立赫南特阶底界的全球界线层型剖面和点位的提案报告于2004年10月被国际地层委员会奥陶系分会通过,经补充完善后,于2006年2月被国际地层委员会通过,同年5月被国际地科联正式批准。 展开更多
关键词 奥陶系 赫南特阶 全球界线层型剖面和点位(GSSP)
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