期刊文献+

湘西-鄂西成矿带新元古代地层区划及岩石地层划分对比方案 被引量:2

The subregion, division and correlation of the Neoproterozoic stratigraphy of Western Hunan-Hubei metallogenic belt
在线阅读 下载PDF
导出
摘要 湘西—鄂西成矿带自新太古界至第四系均有发育。依据大地构造演化特征,结合地层发育特征及岩相古地理,按青白口纪和南华纪—震旦纪两个阶段进行地层区划分。青白口纪时期,研究区分为南秦岭地层区、黄陵地层区、梵净山地层区、武陵-雪峰地层区与四川盆地区。南华纪-震旦纪时期,研究区分为南秦岭地层区武当地层分区、陨均台地层分区及扬子地层区湘黔鄂地层分区、湘中分区。对成矿带岩石地层提出了对比方案,主要为:石桥铺组和黄狮洞组来替代甲路组;沿用乌叶组而弃用砖墙湾组;重新定义清水江组,将以板岩为主的地层都归属清水江组,相当于番召组上段、清水江组、平略组之和;保留原清水江组之上的隆里组而弃用平略组(黔)和岩门寨组(湘);弃用陨均台地区的"陡山沱组"和"灯影组",沿用尚家店组和青山寨组的定名;采用老堡组来替代留茶坡组。 The stratigraphy of Western Hunan-Hubei metallogenic belt has developed since the Neoarchean to Quaternary period. According to the characteristics of geotectonic evolution, stratigraphy and lithofacies palaeogeography, we divide the Neoproterozoic stata of the area into the Qingbaikou stage and Nanhua-Sinian stage.During the Qingbaikou stage, the metallogenic belt is divided into five stratigraphic regions called Southern Qinling, Huangling, Fanjingshan, Wuling-Xuefeng and Sichuan basin, respectively. During the Nanhua-Sinian stage,the belt is divided into Southern Qinling stratigraphic region(including Wudang and Yunjuntai stratigraphic subregion) and Yangtze stragraphic region(including Hunan-Guizhou-Hubei and Central Hunan stratigraphic subregion). We also recommende to adopt or redifine some stratigraphic units. Keep Huangshidong Formation and Shiqiaopu Formation instead of Jialu Formation, use Wuye Formation and discard Zhuanqiangwan Formation.Qingshuijiang Formation is redefined to describe the main slate strata and equivalent of the combination of the upper part of Fanzhao Formation, Qingshuijiang Formation, Pinglue Formation. Disuse Pinglue Formation(Guizhou)and Yanmenzhai Formation(Hunan) and keep Longli Formation. The "Doushantuo Formation"and"Dengying Formation"in the Yunxian and Yunxi area are replaced by "Shangjiadian Formation"and "Qingwangzhai Formation", respectively. Disuse"Liuchapo Formation"and persist"Laobao Formation".
出处 《华南地质与矿产》 CAS 2014年第4期299-307,共9页 Geology and Mineral Resources of South China
基金 中国地质调查局"湘西-鄂西成矿带关键地区地质调查"项目(编号:12120113061700) "武当-桐柏-大别成矿带关键地区地质调查"项目(编号:12120113067900)
关键词 新元古代 地层划分与对比 地层分区 岩相古地理 湘西-鄂西成矿带 Neoproterozoic stratigraphic division and correlation stratigraphic region lithofacies-paleogeography Western Hunan-Hubei metallogenic belt
  • 相关文献

参考文献32

二级参考文献237

共引文献748

同被引文献30

  • 1饶家荣,王纪恒,曹一中.湖南深部构造[J].湖南地质,1993(A08):1-101. 被引量:129
  • 2王剑.华南“南华系”研究新进展——论南华系地层划分与对比[J].地质通报,2005,24(6):491-495. 被引量:89
  • 3黄建中,唐晓珊,张晓阳,郭乐群.对峡东莲沱组与湖南板溪群对比问题的一点浅见[J].地层学杂志,1996,20(3):232-236. 被引量:11
  • 4王剑,曾昭光,陈文西,汪正江,熊国庆,王雪华.华南新元古代裂谷系沉积超覆作用及其开启年龄新证据[J].沉积与特提斯地质,2006,26(4):1-7. 被引量:83
  • 5饶家荣,等.桃江-城步壳下岩石圈碰撞断裂带及其地质意义[C].湖南地学新进展.湖南科学技术出版社,1996.
  • 6Compston W, Williams I S, Kirschvink J L, Zhang Z C, Ma GG. Zircon U-Pb ages of the early Cambrian time-scale [J].Journal of the Geological Society, 1992, 149(2):171-184.
  • 7Williams I S, Claesson S. Isotope evidence for the Precambrianprovince and Caledonian metamorphism of high gradeparagneiss from the Seve Nappes, Scandinavian Caledonides[J]. Contributions to Mineralogy and Petrology,1987,97 (2):205-217.
  • 8Ludwig K R. SQUID 1.02: A User’s Manual [M]. Berkeley:Berkeley Geochronology Center Special Publication, 2001.
  • 9Ludwig K R. User’s Manual for Isoplot 3.00: A GeochronologicalToolkit for Microsoft Excel [M]. Berkeley: BerkeleyGeochronology Center, Special Publication, 2: 1-19.
  • 10Qi D, Wang J, Wang Z J, Wang X C, Qiu Y S, Yang Q X, DuQ D, Cui X Z, Zhou X L. Continental flood basalts of theHuashan Group, northern margin of the Yangtze blockimplications for the breakup of Rodinia[J]. International GeologyReview, 2013, 55(15):1865-1884.

引证文献2

二级引证文献18

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部