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浙江桐庐阳新统栖霞组的(竹蜓)类化石及多重地层划分
引用本文:颜铁增,朱朝晖,卢成忠,许兴苗.浙江桐庐阳新统栖霞组的(竹蜓)类化石及多重地层划分[J].地层学杂志,2007,31(1):79-89.
作者姓名:颜铁增  朱朝晖  卢成忠  许兴苗
作者单位:浙江省地质调查院,浙江杭州,311203
基金项目:中国地质调查局1/25万<金华市幅>国土资源大调查项目
摘    要:浙江桐庐栖霞组可划分为二个(竹蜓)带:上部为Cancellina neoschwagerinoides-Verbeekina grabaui带,归属祥播阶;下部为Misellina claudiae带,归属罗甸阶.栖霞组被划分出3个正层序和6个四级层序.高频旋回层研究表明:栖霞组主要的成岩环境有台地相、浅海陆棚相和盆地相三种类型,从下至上总体反映为台地向盆地的演化环境.

关 键 词:(竹蜓)化石带  阳新统  二叠系  栖霞组  多重地层划分  桐庐  浙江
文章编号:0253-4959(2007)01-0079-11
修稿时间:04 4 2006 12:00AM

FUSULINIDS AND STRATIGRAPHIC SUBDIVISION OF THE QIXIA FORMATION OF THE YANGXIN SERIES IN THE TONGLU AREA, ZHEJIANG
YAN Tie-zeng,ZHU Chao-hui,LU Cheng-zhong,XU Xing-miao.FUSULINIDS AND STRATIGRAPHIC SUBDIVISION OF THE QIXIA FORMATION OF THE YANGXIN SERIES IN THE TONGLU AREA, ZHEJIANG[J].Journal of Stratigraphy,2007,31(1):79-89.
Authors:YAN Tie-zeng  ZHU Chao-hui  LU Cheng-zhong  XU Xing-miao
Institution:Zhejiang Geological Survey, Hangzhou , 311203
Abstract:The Qixia Formation in the Tonglu area of Zhejiang Province can be divided into two fusulinid biozones.the upper Cancellina neoschwagerinoides-Verbeekina grabaui zone of the Xiangbo Stage and the lower Misellina claudiae zone of the Luodian Stage. The Qixia Formation includes three 3rd-order sequences and six 4th-order sequences. On the basis of sedimentary cycles of the Qixia Formation ,three depositional facies can be recognized.platform facies, shallow sea continental shelf facies and basinal facies. The Qixia Formation records a deepening upward sequence,shifting from platform to basin facies.
Keywords:fusulinid biozone  Yangxin Series  Permian System  Qixia Formation  multi-stratigraphic subdivision  Tonglu  Zhejiang
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