浙江煤山D剖面二叠系长兴组高精度岩石地层HIGH-RESOLUTION LITHOSTRATIGRAPHY OF THE CHANGHSINGIAN STAGE IN MEISHAN SECTION D,ZHEJIANG
曹长群,郑全锋
摘要(Abstract):
基于对浙江煤山D剖面长兴组到下三叠统殷坑组岩石地层单元高精度的测量,选择了Yinetal.(1996)、盛金章等(1987)和赵金科等(1981)的地层资料,对比并修订了早期地层资料中的误差。重点标注了该剖面特殊岩性段,如黏土岩、碳酸盐化流纹质凝灰岩的产出层位,详尽描述了二叠系-三叠系界线附近的微观岩石地层特征,认为Y24e层顶部至Y27层为存在高度凝缩沉积或者沉积缺失的层段。这些高精度岩石地层材料将进一步推动二叠纪-三叠纪过渡期生物灭绝事件的后层型研究。
关键词(KeyWords): 煤山D剖面;长兴组;二叠系;岩石地层
基金项目(Foundation): 国家自然科学基金委员会创新群体项目(40321202);; 中国科学院国际合作重点项目(GJHZ0521)资助
作者(Author): 曹长群,郑全锋
参考文献(References):
- 何锦文.1981.长兴阶层型剖面及殷坑组底部的黏土矿物——兼论二叠、三叠系的分界.地层学杂志,5(3):197—206
- 芮琳,江纳言.1984.苏浙皖地区二叠纪末、三叠纪初的岩相和生物相.古生物学报,32(3):286—296
- 杨万容,江纳言.1980.浙江长兴长兴组火山岩和放射虫的发现.地层学杂志,4(1):67—70
- 杨万容,江纳言.1981.浙江长兴组和二叠-三叠系界线的沉积特征及微相.中国科学院南京地质古生物研究所丛刊,2:113—133
- 盛金章,陈楚震,王义刚,芮琳,廖卓庭,何锦文,江纳言,王成源.1987.苏浙皖地区二叠系和三叠系界线研究的新进展.见:中国科学院南京地质古生物研究所编.二叠系与三叠系界线(一).南京:南京大学出版社.1—21
- 王,曹长群,尚庆华,金玉.2004.二叠系乐平统——一个国际标准年代地层单位.地层古生物论文集,28:135—146
- 殷鸿福,吴顺宝.1985.过渡层——华南三叠系的底界.地球科学——武汉地质学院学报,地层古生物专集(),10(特刊):163—173
- 殷鸿福,丁梅华,张克信,童金南,杨逢清,赖旭龙.1995.扬子及其周缘东吴—印支期生态地层学.北京:科学出版社.1—337
- 张克信,童金南,殷鸿福,吴顺宝.1996.浙江长兴二叠系-三叠系界线剖面层序地层学.地质学报,70(3):270—281
- 赵金科,盛金章,姚兆奇,梁希洛,陈楚震,芮琳,廖卓庭.1981.中国南部的长兴阶和二叠系与三叠系之间的界线.中国科学院南京地质古生物研究所丛刊,2:1—95
- Bowring S A,Erwin D H,Jin Y G,Martin K D&Wang W.1998.U/Pb Zircon geochronology and tempo of the end-Permian massextinction.Science,280:1039—1045
- Cao Chang-qun&Shang Qing-hua.1998.Microstratigraphy of Per-mo-Triassic transitional sequence of the Meishan section,Zhe-jiang,China.Palaeoword,9:147—152
- Claoue-Long J C,Zhang Zi-chao,Ma Guo-gan&Du Shao-hua.1991.The age of the Permian-Triassic boundary.Earth andPlanetary Science Letters,105(1-3):182—190
- Mundil R,Ludwig K R,Metcalfe Ian&Renne P R.2004.Age andtiming of the Permian mass extinctions:U/Pb dating of closed-system Zircons.Science,305:1760—1763
- Mundil R,Metcalfe Ian,Ludwig K R,Renne P R,Oberli F&Nicoll R S.2001.Timing of the Pemrian-Triassic biotic crisis:implications from new zircon U/Pb age data(and their limita-tions).Earth and Planetary Science Letters,187:131—145
- Renne P R,Zhang Zi-chao,Richards M A,Michael T B&Basu AR.1995.Synchrony and causal relations between Permian-Tri-assic boundary crises and Siberian flood volcanism.Science,269:1413—1415
- Sheng Jin-zhang,Chen Chu-zhen,Wang Yi-gang,Rui Lin,LiaoZhuo-ting,Bando Y,Ishii K I,Nakazawa K&Nakamura K.1984.Permian-Triassic boundary in middle and easternTethys.Jour.Fac.Sci.Hokkaido Univ.,4:133—181
- Twitchett J R,Looy V C,Morante R,Visscher H&Wignall B P.2001.Rapid and synchronous collapse of marine and terrestrialsystems during the end-Permian biotic crisis.Geology,29(4):351—354
- Yin Hong-fu,Wu Shun-bao,Ding Mei-hua,Zhang Ke-xin,TongJin-nan,Yang Feng-qing&Lai Xu-long.1996.The Meishansection,candidate of the global stratotype section and point ofPermian-Triassc boundary.In:Yin Hong-fu et al.eds.ThePalaeozoic-Mesozoic boundary candidates of Global StratotypeSection and Point of the Permian-Triassic boundary(NSFC pro-ject).Wuhan:China University of Geosciences Press.31—48
- Zhang Ke-xin,Lai Xu-long,Ding Mei-hua,Wu Shun-bao&LiuJin-hua.1995.Conodont sequence and its global correlation ofPermian-Triassic boundary in Meishan section,Changxing,Zhejiang Province.Earth Science——Journal of China Univer-sity of Geosciences,20(6):669—676