华南下扬子区下奥陶统仑山组:岩石学、地层学和古地理学<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2016.03.029

古地理学报 ›› 2016, Vol. 18 ›› Issue (3): 411-423. doi: 10.7605/gdlxb.2016.03.029

• 岩相古地理学及沉积学 • 上一篇下一篇

华南下扬子区下奥陶统仑山组:岩石学、地层学和古地理学^*

李家腾¹, 刘建波¹, 孙永超¹, 闫振¹, 吴荣昌², 詹仁斌²

1 北京大学地球与空间科学学院,造山带与地壳演化教育部重点实验室(北京大学), 北京 100871;
2 现代古生物学和地层学国家重点实验室,中国科学院南京地质古生物研究所,江苏南京 210008;

收稿日期:2015-07-20 修回日期:2015-09-21 出版日期:2016-06-01 发布日期:2016-06-01
通讯作者: 刘建波,男,1966年生,北京大学地球与空间科学学院教授,主要研究方向为古生物学、沉积学和地球生物学。E-mail: jbliu@pku.edu.cn。 E-mail:lijiateng@pku.edu.cn。
作者简介:李家腾,男,1992年生,北京大学硕士研究生,主要研究方向为沉积学。
基金资助:
*国家自然科学基金项目(批准号:41272035,41221001,41290260)和现代古生物学和地层学国家重点实验室共同资助

On the Lower Ordovician Lunshan Formation in Lower Yangtze Region, South China:Its petrology, stratigraphy and palaeogeography

Li Jiateng¹, Liu Jianbo¹, Sun Yongchao¹, Yan Zhen¹, Wu Rongchang², Zhan Renbin²

1 School of Earth and Space Sciences,Peking University,Key Laboratory of Orogenic Belts;and Crustal Evolution, Ministry of Education, Beijing 100871;
2 State Key Laboratory of Palaeobiology and Stratigraphy,Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing 210008,Jiangsu

Received:2015-07-20 Revised:2015-09-21 Online:2016-06-01 Published:2016-06-01
Contact: Liu Jianbo,born in 1966,is a professor in Peking University. He is mainly engaged in paleontology,sedimentology and geobiology. E-mail: jbliu@pku.edu.cn. E-mail:lijiateng@pku.edu.cn。
Supported by:
Co-funded by the National Natural Science Foundation of China(Grant No.41272035,41221001,41290260)and the foundation of the State Key Laboratory of Palaeobiology and Stratigraphy

摘要/Abstract

摘要： 华南地区下奥陶统仑山组为奥陶系最底部的岩石地层单位之一,其以大套白云岩为主要特征,广泛分布于下扬子区。通过对安徽池州洪家剖面仑山组的系统分析,并结合下扬子区多个相关剖面的资料,进一步确定仑山组岩性为白云岩、灰质白云岩和白云质灰岩,夹有部分亮晶颗粒灰岩和亮泥晶颗粒灰岩。整体上以亮晶生屑灰岩或泥晶生屑灰岩的出现作为仑山组顶界,在下扬子区内部、北部及东南部地区以白云质灰岩或灰质白云岩出现为其底界,而在下扬子区西南部大部分地区则以白云岩化出现为其底界。整个仑山组所含生物化石种类和数量较少,自下而上可建立5个牙形石带,分别是Monocostatus sevierensis带、Acanthodus lineatus-A. costatus带、Scolopodus? pseudoplanus带、Glyptoconus quadraplicatus带和Paltodus deltifer-Tripodus proteus带,推测其时代为早奥陶世特马豆克早期。仑山组主要形成于浅潮下带至深潮下带环境中,其地层总厚度和其中的白云岩厚度受到古地理因素的控制。通过岩石学特征分析,推断仑山组白云岩主要为准同生条件下的多种白云岩化作用叠加中等埋藏条件下的白云岩化形成。

关键词: 地层学, 古地理学, 白云岩, 仑山组, 下奥陶统, 下扬子区

Abstract: The Lunshan Formation is one of the lowest stratigraphic units of the Lower Ordovician in the Lower Yangtze Region in South China. The formation is characterized by massive dolostone in comparison with other contemporaneous lithological units,and extends widely. A detailed analysis on the Lunshan Formation at Hongjia section of Chizhou County, Anhui Province, as well as a comprehensive review of the previous studies, indicates that the Lunshan Formation consists of dolostone,lime dolostone,dolomitic limestone,and minor,intercalated grainstone and packstone. The upper boundary of the formation is marked by the occurrence of medium- to thick-bedded bioclastic grainstone and packstone in the study area. The lower boundary of the formation is marked by occurrence of dolomitic limestone or lime dolostone in inner,northern and southeastern Lower Yangtze Region and occurrence of dolostone in most parts of southern Lower Yangtze Region. Although fossils are commonly rare in the Lunshan Formation,five conodont biozones are established in an ascending order:Monocostatus sevierensis biozone,Acanthodus lineatus-A. costatus biozone, Scolopodus? pseudoplanus biozone, Glyptoconus quadraplicatus biozone,and Paltodus deltifer-Tripodus proteus biozone, corresponding to the early Tremadocian of Early Ordovican. The Lunshan Formation was deposited in shallow subtidal to deep subtidal settings. The spatial changes in the thickness of the formation as well as those of dolostone were mainly controlled by palaeogeographic factors. The sedimentary properties of dolomite in the Lunshan Formation imply that these dolostones were mostly formed by penecontemporaneous dolomitization superimposed with moderate burial dolomitization.

Key words: stratigraphy, palaeogeography, dolostone, Lunshan Formation, Lower Ordovician, Lower Yangtze Region

中图分类号:

P531

李家腾, 刘建波, 孙永超, 闫振, 吴荣昌, 詹仁斌. 华南下扬子区下奥陶统仑山组:岩石学、地层学和古地理学^*[J]. 古地理学报, 2016, 18(3): 411-423.

Li Jiateng, Liu Jianbo, Sun Yongchao, Yan Zhen, Wu Rongchang, Zhan Renbin. On the Lower Ordovician Lunshan Formation in Lower Yangtze Region, South China:Its petrology, stratigraphy and palaeogeography[J]. JOPC, 2016, 18(3): 411-423.

http://www.gdlxb.cn/CN/Y2016/V18/I3/411

参考文献

[1] 安徽省地质矿产局. 1987. 安徽省区域地质志. 北京:地质出版社,63-270. [Department of Geology and Mineral Resources of Anhui Province. 1987. Regional Geology of Anhui Province. Beijing:Geological Publishing House,63-270]
[2] 安徽省地质矿产局. 1989. 安徽地层志·奥陶系分册. 安徽合肥:安徽科技出版社,10-188. [Department of Geology and Mineral Resources of Anhui Province. 1989. Geology of Anhui:Ordovician. Aahui Hefei:Anhui Science and Technology Press,10-188]
[3] 安太庠. 1987. 中国南部早古生代牙形石. 北京:北京大学出版社,16-70. [An T X. 1987. The Lower Paleozoic Conodonts of South China. Beijing:Peking University Press,16-70]
[4] 安太庠,丁连生. 1982. 宁镇山脉地区奥陶系牙形石的初步研究及对比. 石油学报,(4):1-12. [An T X,Ding L S. 1982. Preliminary studies and correlations on Ordovician conodonts from the Ningzhen Mountains,Nanjing,China. Acta Petrolei Sinica,(4):1-12]
[5] 安太庠,丁连生. 1985. 安徽和县奥陶纪牙形石生物地层研究. 地质论评,31(1):1-12. [An T X,Ding L S. 1985. Ordovician conodonts biostratigraphy in Hexian,Anhui Province. Geological Review,31(1):1-12]
[6] 陈学时. 1992. 皖南寒武—奥陶系白云岩类型及成因探讨. 石油勘探与开发,19(1):13-22. [Chen X S. 1992. Types and origins of Cambrian-Ordovician dolomite in Southern Anhui. Petroleum Exploration and Development,19(1):13-22]
[7] 丁连生. 1987. 江苏昆山地区奥陶纪牙形石生物地层探讨. 见:石油地层古生物会议论文集编委会. 石油地层古生物会议论文集. 北京:地质出版社,41-53. [Ding L S. 1987. Preliminary probes into Ordovician conodont biostratigraphy from the Kunshan area,Jiangsu,China. In:The Editorial Committee of the Petrolei Symposium on Stratigraphy and Palaeontology. Papers for the Petrolei Symposium on Stratigraphy and Palaeontology. Beijing:Geological Publishing House,41-53]
[8] 丁连生,安太庠. 1985. 杭州余杭荆山岭奥陶纪牙形石及其地质意义. 见:北京大学地质学系. 地质研究论文集. 北京:北京大学出版社,11-19. [Ding L S,An T X. 1985. Ordovician conodonts from Jingshanling,Zhejiang and their geological significance. In:Department of Geology,Peking University. The Records of Geological Research. Beijing:Peking University Press,11-19]
[9] 丁文江. 1919. 芜湖以下扬子江流域地质报告. 见:黄汲清(主编). 丁文江文集. 北京:北京大学出版社,80-124. [Ding W J. 1919. Report on the geology of the Yangtze Valley below Wuhu. In:Huang J Q(chief editor). A Collection of Works by V.K.Ting. Beijing:Peking University Press,80-124]
[10] 段金英. 1990. 苏北地区奥陶系牙形刺及其色变指标. 微体古生物学报,7(1):19-41,99-103. [Duan J Y. 1990. Ordovician conodonts from Northern Jiangsu and indices of their color alteration. Acta Micropalaeontologica Sinica,7(1):19-41,99-103]
[11] 范德江,栾光忠,李师汤,郭志刚. 1996. 南京汤山上震旦统及古生界白云岩成因初探. 海洋湖沼通报,(3):26-32. [Fan D J,Luan G Z,Li S T,Guo Z G. 1996. The origin of dolostones appear in Upper-Sinian and Paleozoic,Tangshan,Nanjing. Transaction of Oceanology and Limnology,(3):26-32]
[12] 冯洪真,李明,张元动,Erdtmann B D,李丽霞,王文卉. 2009. 华南上特马道克阶的笔石带序列及其全球对比. 中国科学D辑:地球科学,39(5):556-568. [Feng H Z,Li M,Zhang Y D,Erdtmann B D,Li L X,Wang W H. 2009. Succession and global correlation of Late Tremadoc graptolite zones from South China. Science in China Series D: Earth Science,39(5):556-568]
[13] 冯增昭,彭勇民,金振奎,鲍志东. 2003. 中国早奥陶世岩相古地理. 古地理学报,5(1):1-16. [Feng Z Z,Peng Y M,Jin Z K,Bao Z D. 2003. Lithofacies palaeogeography of the Early Ordovician in China. Journal of Palaeogeography(Chinese Edition),5(1):1-16]
[14] 何炎,梁希洛,张肇诚,胡兆珣,陈旭,赵嘉明. 1964. 安徽长江沿岸古生代及三叠纪地层. 见:穆恩之. 中国科学院地质古生物研究所集刊. 北京:科学出版社,4:171-201. [He Y,Liang X L,Zhang Z C,Hu Z X,Chen X,Zhao J M. 1964. The Paleozoic and Triassic in the regions along the Yangtze River. In:Mu E Z. Collected Papers of the Institute of Geology and Palaeontology,Chinese Academy of Sciences. Beijing:Science Press,4:171-201]
[15] 江苏省地质矿产局. 1984. 江苏省及上海市区域地质志. 北京:地质出版社,122-126. [Department of Geology and Mineral Resources of Jiangxi Province. 1984. Monograph on the Regional Geology of Jiangsu Province and Shanghai City,People��s Republic of China. Beijing:Geological Publishing House,122-126.]
[16] 江西省地质矿产厅. 1997. 全国地层多重划分对比研究江西省岩石地层. 湖北武汉:中国地质大学出版社,83-84. [Department of Geology and Mineral Resources of Jiangxi Province. 1997. Multiple Classification and Correlation of the Stratigraphy of China,Stratigraphy(Lithostratic)of Jiangxi Province. Hubei Wuhan:China University of Geosciences Press,83-84]
[17] 江西省区域地层表编写组. 1980. 华东地区区域地层表江西省分册. 北京:地质出版社,13-14. [Writing Group of Regional Stratigraphic Chart of Jiangxi Province. 1980. Regional Stratigraphic Chart of East China:Jiangxi. Beijing:Geological Publishing House,13-14]
[18] 赖才根,金若谷,林宝玉,黄枝高. 1993. 下扬子地区奥陶纪生物相、沉积相及古地理特征. 北京:地质出版社,2-80. [Lai C G,Jin R G,Lin B Y,Huang Z G. 1993. Biofacies,Sedimentary Facies and Palaeogeographic Characteristics of the Ordovician in the Lower Yangtze Area. Beijing:Geological Publishing House,2-80]
[19] 李毓尧,李捷,朱森. 1935. 宁镇山脉地质. 见:前中央研究院地质研究所. 前中央研究院地质研究所集刊,11:4-7. [Li Y Y,Li J,Zhu S. 1935. Geology of Ningzhen Mountains. In:The Institute of Geology of the Former Academia Sinica. Memoirs of the Institute of Geology of the Former Academia Sinica,11:4-7]
[20] 廖翰卿,刘建波,吴荣昌,孙永超,詹仁斌. 2013. 华南上扬子区下奥陶统红花园组顶界的穿时性. 古生物学报,52(1):18-34. [Liao H Q,Liu J B,Wu R C,Sun Y C,Zhan R B. 2013. Phenomenal diachroneity in the upper boundary of the Lower Ordovician Hunghuayuan Formation in the Upper Yangtze Region,South China. Acta Palaeontologica Sinica,52(1):18-34]
[21] 梁薇,牟传龙,周恳恳,葛祥英,陈超,徐鹏辉. 2015. 中上扬子地区寒武纪第三世—芙蓉世古地理. 古地理学报,17(2):172-185. [Liang W,Mou C L,Zhou K K,Ge X Y,Chen C,Xu P H. 2015. Palaeogeography of the Cambrian Epoch 3-Furongian in the Middle and Upper Yangtze Region. Journal of Palaeogeography(Chinese Edition),17(2):172-185]
[22] 罗以达,俞国华,张岩,梁河,陈小友,吴鸣. 2008. 浙江杭州地区中下奥陶统岩石地层研究. 中国地质,35(4):648-655. [Luo Y D,Yu G H,Zhang Y,Liang H,Chen X Y,Wu M. 2008. Middle-Lower Ordovician lithostratigraphy in the Hangzhou area,Zhejiang. Geology in China,35(4):648-655]
[23] 马永生,陈洪德,王国力. 2009. 中国南方层序地层与古地理学. 北京:科学出版社,2-266. [Ma Y S,Chen H D,Wang G L. 2009. Sequence Stratigraphy and Paleogeography in South China. Beijing:Science Press,2-266]
[24] 穆恩之,潘江,俞昌民. 1955. 南京汤山奥陶纪地层新知. 地质知识,1:23-24. [Mu E Z,Pan J,Yu C M. 1955. New knowledge of Ordovician at Tangshan,Nanjing. Geological Knowledge,1:23-24]
[25] 潘江. 1956. 宁镇山脉古生代地层的新认识. 地质学报,36(1):1-23. [Pan J. 1956. On the Paleozoic stratigraphy of the Nanking Hills. Acta Geologica Sinica,36(1):1-23]
[26] 齐敦伦,杜森官. 1981. 安徽无为、含山一带的奥陶系. 地层学杂志,5(1):20-27. [Qi D L,Du S G. 1981. Ordovician in Wuwei and Hanshan area,Anhui. Journal of Stratigraphy,5(1):20-27]
[27] 钱义元,李积金,李蔚秾,江纳言,毕治国,高永修. 1964. 安徽南部震旦系及下古生界的新认识. 见:中国科学院. 中国科学院南京地质古生物研究所集刊. 北京:科学出版社, 21-66. [Qian Y Y,Li J J,Li W N,Jiang N Y,Bi Z G,Gao Y X. 1964. A revision of Sinian and Lower Paleozoic in Southern Anhui,China. In:Chinese Academy of Sciences. Collected Papers of Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences. Beijing:Science Press, 21-66]
[28] 唐增才,张元动,甄勇毅,胡文杰,袁强,俞国华. 2014. 浙江临安板桥早奥陶世牙形刺新材料及其意义. 地层学杂志,38(4):381-389. [Tang Z C,Zhang Y D,Zhen Y Y,Hu W J,Yuan Q,Yu G H. 2014. New material of Early Ordovician conodonts from the Banqiao Section,Lin��an,Zhejiang and their biostratigraphic significance. Journal of Stratigraphy,38(4):381-389]
[29] 王兵杰,蔡明俊,林春明,张霞,程远忠,曲长伟,张妮. 2014. 渤海湾盆地塘沽地区古近系沙河街组湖相白云岩特征及成因. 古地理学报,16(1):65-76. [Wang B J,Cai M J,Lin C M,Zhang X,Cheng Y Z,Qu C W,Zhang N. 2014. Characteristics and origin of lacustrine dolostone of the Paleogene Shahejie Formation in Tanggu area,Bohai Bay Basin. Journal of Palaeogeography(Chinese Edition),16(1):65-76]
[30] 王钰,许汉奎. 1966. 江苏宁镇山脉的早奥陶世腕足动物. 古生物学报,14(1):62-81. [Wang Y,Xu H K. 1966. Some Lower Ordovician brachiopods from Tangshan,Nanjing,Jiangsu. Acta Palaeontologica Sinica,14(1):62-81]
[31] 王志浩,吴荣昌. 2009. 下扬子区奥陶纪牙形刺多样性演变初探. 微体古生物学报,26(4):331-350. [Wang Z H,Wu R C. 2009. Ordovician conodont diversification of the Lower Yangtze Valley. Acta Micropalaeontologica Sinica,26(4):331-350]
[32] 吴荣昌,詹仁斌,李贵鹏,刘建波. 2007. 浅论华南扬子区下、中奥陶统紫台组. 地层学杂志,31(4):325-332. [Wu R C,Zhan R B,Li G P,Liu J B. 2007. Brief discussion on the lower to middle Ordovician Zitai Formation in the Yangtze Region,South China. Journal of Stratigraphy,31(4):325-332]
[33] 许汉奎. 1976. 江苏宁镇山脉仑山灰岩的新认识. 地质科学,(3):235-245. [Xu H K. 1976. New recognition of the Lunshan Limestone in the Nanjing Hills,Southern Jiangsu. Scientia Geologica Sinica,(3):235-245]
[34] 俞国华,包超民,方炳兴,马武平,宋福泉,何圣策. 1995. 浙江省岩石地层清理成果简介. 浙江地质,11(1):1-13. [Yu G H,Bao C M,Fang B X,Ma W P,Song F Q,He S C. 1995. Brief introduction to the achievements on lithostratigraphic clearing in Zhejiang. Geology of Zhejiang,11(1):1-13]
[35] 俞建章. 1933. 南京附近仑山石灰岩与湖北奥陶纪地层之比较. 见:前中央研究院地质研究所. 前中央研究院地质研究所集刊,3:5-45. [Yu J Z. 1933. The correlation of Lunshan Limestone around Nanjing and Ordovician in Hubei. In:The Institute of Geology of the Former Academia Sinica. Memoirs of the Institute of Geology of the Former Academia Sinica,3:5-45]
[36] 俞剑华,陈敏娟,黄志诚,方一亭,陈云棠. 1979. 江苏南部的奥陶系. 地层学杂志,3(3):157-174,233-234. [Yu J H,Chen M J,Huang Z C,Fang Y T,Chen Y T. 1979. Ordovician in Southern Jiangsu. Journal of Stratigraphy,3(3):157-174,233-234]
[37] 袁鑫鹏,刘建波. 2012. 回流渗透模式白云岩研究历史与进展. 古地理学报,14(2):219-228. [Yuan X P,Liu J B. 2012. Research history and progress on reflux seepage dolostone. Journal of Palaeogeography(Chinese Edition),14(2):219-228]
[38] 袁鑫鹏,刘建波. 2013. 湖北兴山古洞口剖面中—上寒武统白云岩特征及其古环境意义. 古地理学报,15(3):363-382. [Yuan X P,Liu J B. 2013. Characteristics and its palaeoenvironmental significance of the Middle-Upper Cambrian dolostones of Gudongkou section at Xingshan,Hubei Province. Journal of Palaeogeography(Chinese Edition),15(3):363-382]
[39] 岳文浙,魏乃颐,焦世鼎,姜月华. 1990. 下扬子地区寒武、奥陶纪陆棚—斜坡相沉积特征和相模式(研究报告). 见:南京地质矿产研究所. 中国地质科学院南京地质矿产研究所所刊, 8:3-46. [Yue W Z,Wei N Y,Jiao S D,Jiang Y H. 1990. Sedimentary characteristics and facies model of shelf to slope environments in the Cambrian-Ordovician of Lower Yangtze Area(Research report). In:Nanjing Institute of Geological Mineral Resource. Bulletin of Nanjing Institute of Geological Mineral Resource,Chinese Academy of Geological Sciences, 8:3-46]
[40] 张德民,鲍志东,潘文庆,郝雁,陈敏. 2013. 塔里木盆地下古生界白云岩类型及成因. 古地理学报,15(5):693-706. [Zhang D M,Bao Z D,Pan W Q,Hao Y,Chen M. 2013. Type and origin of the Lower Paleozoic dolostones in Tarim Basin. Journal of Palaeogeography(Chinese Edition),15(5):693-706]
[41] 张国伟,郭安林,王岳军,李三忠,董云鹏,刘少峰,何登发,程顺有,鲁如魁,姚安平. 2013. 中国华南大陆构造与问题. 中国科学:地球科学,43(10):1553-1582. [Zhang G W,Guo A L,Wang Y J,Li S Z,Dong Y P,Liu S F,He D F,Cheng S Y,Lu R K,Yao A P. 2013. Tectonics of South China continent and its implications. Scientia Sinica Terrae,43(10):1553-1582]
[42] 张举,张元动,宋妍妍. 2013. 滇东地区奥陶系红石崖组的时代. 地层学杂志,37(1):8-17. [Zhang J,Zhang Y D,Song Y Y. 2013. Graptolite fauna and age of the Hungshihyen Formation(Ordovician)in Eastern Yunnan,Southwest China. Journal of Stratigraphy,37(1):8-17]
[43] 张元动,王志浩,冯洪真,骆天天,Erdtmann B D. 2005. 中国特马豆克阶笔石地层述评. 地层学杂志,29(3):215-235. [Zhang Y D,Wang Z H,Feng H Z,Luo T T,Erdtmann B D. 2005. Tremadocian(Ordovician)graptolite biostratigraphy of China:A review. Journal of Stratigraphy,29(3):215-235]
[44] 张允白,周志毅,张俊明. 2002. 扬子陆块早奥陶世末期—中奥陶世Darriwilian初期沉积分异. 地层学杂志,26(4):302-314. [Zhang Y B,Zhou Z Y,Zhang J M. 2002. Sedimentary differentiation during the latest Early Ordovician-earliest Darriwilian in the Yangtze Block. Journal of Stratigraphy,26(4):302-314]
[45] 赵锐,吴亚生,齐恩广,姜红霞. 2014. 川东北上二叠统长兴组白云岩地球化学特征及形成机制. 古地理学报,16(5):747-760. [Zhao R,Wu Y S,Qi E G,Jiang H X. 2014. Geochemistry and origin of dolomites of the Upper Permian Changxing Formation in northeastern Sichuan Basin. Journal of Palaeogeography(Chinese Edition),16(5):747-760]
[46] 周名魁,王汝植,李志明. 1993. 中国南方奥陶—志留纪岩相古地理与成矿作用. 北京:地质出版社,2-55. [Zhou M K,Wang R Z,Li Z M. 1993. Ordovician to Silurian Lithofacies,Paleogeography and Mineralization in South China. Beijing:Geological Publishing House,2-55]
[47] Li Y,Kershaw S,Mu X. 2004. Ordovician reef systems and settings in South China before the Late Ordovician mass extinction. Palaeogeography,Palaeoclimatology,Palaeoecology,205:235-254.
[48] Machel H G. 2004. Concepts and models of dolomitization:A critical reappraisal. In:Braithwaite C J R,Rizzi J,Darke G. The Geometry and Petrogenesis of Dolomite Hydrocarbon Reservoirs. London:Geological Society Special Publications,235:7-63.
[49] Warren J. 2000. Dolomite:Occurrence,evolution and economically important associations. Earth-Science Reviews,52(1-3):1-81.
[50] Zhan R B,Jin J S. 2007. Ordovician-Silurian(Llandvery)Stratigraphy and Palaeontology of the Upper Yangtze Platform,South China. Beijing:Science Press,11-14.

选择文件类型/文献管理软件名称

选择包含的内容

华南下扬子区下奥陶统仑山组:岩石学、地层学和古地理学^*

On the Lower Ordovician Lunshan Formation in Lower Yangtze Region, South China:Its petrology, stratigraphy and palaeogeography

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	刘大卫, 李映涛, 韩俊, 张继标, 汝智星, 杨孝群, 王石, 黄诚, 肖重阳. 塔里木盆地顺北地区奥陶系鹰山组超深层白云岩类型及成储潜力评价^*[J]. 古地理学报, 2025, 27(1): 126-140.
[2]	李阳. 鄂尔多斯盆地南缘旬探1井奥陶系天文旋回信号提取及三级层序的判识^*[J]. 古地理学报, 2025, 27(1): 209-224.
[3]	汪彦, 王诺宇, 杨德彬, 张恒, 张娟, 张长建, 张晓. 塔河油田西北部奥陶系古水系结构特征及演化^*[J]. 古地理学报, 2024, 26(6): 1467-1482.
[4]	魏世林, 焦鑫, 柳益群, 李红, 周鼎武, 吕亦然. 陆内裂谷湖相火山-热液沉积型白云岩研究进展^*[J]. 古地理学报, 2024, 26(5): 1037-1057.
[5]	李滢, 李飞, 鲁子野, 李杨凡, 王曾俊, 李雅兰, 谢慧, 张天舒. 汉南—米仓山地区东部寒武系仙女洞组斑块白云岩特征及形成机制^*[J]. 古地理学报, 2024, 26(5): 1235-1255.
[6]	吴宇婷, 甯濛, 夏攀, 乔占峰, 于洲, 文华国. 白云岩-蒸发岩共生体系白云石化过程研究:以鄂尔多斯盆地马家沟组为例^*[J]. 古地理学报, 2024, 26(4): 895-910.
[7]	丁晓琪, 田胤瑜, 雷涛, 张威, 李晓慧, 高景云. 吕梁古隆起对鄂尔多斯盆地马家沟组沉积的控制作用: 基于陕西府谷剖面^*[J]. 古地理学报, 2024, 26(3): 671-682.
[8]	许红, 张莉, 陈舒, 付和平, 韩超, 马亚增, 苏大鹏. 中国碳酸盐岩油气勘探与白云岩研究最新成果: 第17届全国古地理学及沉积学学术会议成果综述^*[J]. 古地理学报, 2024, 26(2): 475-486.
[9]	李新坡, 郑秀娟, 朱筱敏, 鲍志东, 王媛, 鲜本忠. “古地理学术论坛”第1—17期评述[J]. 古地理学报, 2024, 26(2): 502-508.
[10]	王瑞, 吴律, 余克服, 任敏, 潘立银. 新生代岛礁白云岩的基本特征、发育演化和成因机制^*[J]. 古地理学报, 2023, 25(6): 1277-1298.
[11]	王俊辉, 鲜本忠. 冲积河流平衡的再认识^*[J]. 古地理学报, 2023, 25(5): 1011-1031.
[12]	于洲, 胡子见, 王前平, 赵静, 吴东旭, 吴兴宁, 李维岭, 鲁慧丽, 朱文博. 鄂尔多斯盆地中东部奥陶系深层白云岩储集层特征及主控因素^*[J]. 古地理学报, 2023, 25(4): 931-944.
[13]	张明震, 刘国龙, 戴霜, 陈世强, 李爱静, 交巴顿珠, 张静, 林少华. 甘蒙交界北山地区早白垩世地层梳理及时代归属新见^*[J]. 古地理学报, 2023, 25(2): 497-510.
[14]	时志强, 彭深远, 赵安坤, 葛禹, 李昌昊. 重庆綦江观音桥剖面观音桥层的岩性新认识^*[J]. 古地理学报, 2023, 25(1): 43-55.
[15]	马亚增, 陈舒, 刘震, 王亚如, 魏浩天, 韦志浩, 张子瑾, 许红, 罗进雄. 西沙群岛西科1井三亚组一段致密白云岩围岩矿物及稀土元素特征^*[J]. 古地理学报, 2023, 25(1): 149-162.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

华南下扬子区下奥陶统仑山组:岩石学、地层学和古地理学*

On the Lower Ordovician Lunshan Formation in Lower Yangtze Region, South China:Its petrology, stratigraphy and palaeogeography

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

华南下扬子区下奥陶统仑山组:岩石学、地层学和古地理学^*