JS鼠标移动切换图片
 
贵州六枝—盘县地区早二叠世隆林期■类组合与沉积环境
详细信息   下载全文 | 推荐本文 |
摘要
六枝—盘县地区的早二叠世隆林期地层,相区分异明显、类化石数量巨大。各相区类化石群落特征差异较大:半局限台地相为Staffella-Nankinella-Pisolina;台地边缘生物滩(礁)相为Parafusulina-Pseudofusulina;斜坡-盆地相为Pseudofusulina,进一步划分为近岸碳酸盐上缓坡环境的Staffella-Parafusulina-Wentzellophyllum群落、远岸碳酸盐上缓坡环境的Pamirina-Schwagerina-Pseudofusulina群落、碳酸盐下缓坡环境的Pseudofusulina-Robustoschwagerina-Kepingophyllum群落和盆地环境的Pseudofusulina-Schwagerina-Verbeekiella群落。
        The fusulinid communities are quite variable in the Longlinian(Early Permian) strata in distinct(sedimentary) environments in the Liuzhi-Panxian region,Guizhou: Staffella-Nankinella-Pisolina community in the semi-restricted platform facies;Parafusulina-Pseudofusulina community in the platform-margin organic shoal(reefs) facies,and Pseudofusulina community in the slope-basin facies.Four communities may further be(recognized) for the last one outlined above,including: Staffella-Parafusulina-Wentzellophyllum community in the nearshore upper carbonate ramp environment;Pamirina-Schwagerina-Pseudofusulina community in the offshore upper carbonate ramp environment;Pseudofusulina-Robustoschwagerina-Kepingophyllum community in the lower carbonate ramp environment,and Pseudofusulina-Schwagerina-Verbeekiella community in the basin environment.
引文
[1]陈洪德,曾允孚.右江沉积盆地的性质及演化讨论[J].岩相古地理,1990,11(1):28-37.
    [2]陈洪德,王成善,刘文均,等.华南二叠纪层序地层与盆地演化[J].沉积学报,1999,17(4):529-535.
    [3]覃建雄,曾允孚,陈洪德,等.西南地区二叠纪层序地层及海平面变化[J].岩相古地理,1998,18(1):19-35.
    [4]史晓颖,梅仕龙,孙岩,等.黔南斜坡相区二叠系层序地层序列及其年代地层对比[J].现代地质,1999,13(1):1-10.
    [5]肖传桃,李维锋,李艺斌.中扬子地区二叠纪生态地层学及古地理特征[J].石油学报,1995,16(3):30-36.
    [6]赵锡奎,朱利春,赵冠军,等.黔中早二叠世茅口晚期断裂陆缘层序地层分析[J].沉积学报,1997,15(1):92-97.
    [7]贵州省地质矿产局.贵州省区域地质志[M].北京:地质出版社,1987.277-321.
    [8]陈源仁.生态地层学原理[M].北京:地质出版社,1992.1-125.
    [9]王尚彦,张慧,彭成龙,等.贵州西部古—中生代地层和裂陷槽盆演化[M].北京:地质出版社,2005.
目录
 

© 2004-2012 中国地质图书馆版权所有 京ICP备05064691号 信息技术室维护

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅:66554900、66554949;咨询服务:66554800;科技查新:66554700