期刊文献+

湘鄂西奥陶纪宝塔组灰岩网纹构造成因及沉积环境探讨 被引量:20

On Polygonal Reticulate Structure of the Ordovician Pagoda Formation of the Western Hunan Hubei Area
原文传递
导出
摘要 网纹构造是宝塔组石灰岩地层中非常发育且分布广泛的一种构造形态 ,其成因一直存在争论和疑问。对湘鄂西地区宝塔组灰岩的研究表明 ,网纹构造的形成不是由于胶体凝缩、水下沉积物收缩或生物遗迹等原因 ,而是一种成岩早期形成的准同生变形构造。根据岩石性质及生物特征推断 ,宝塔组网纹状灰岩沉积于正常浪基面以下、风暴浪基面之上 (水深大约 5 0~ 15 0 m) The polygonal reticulate structure is well developed and wide spread in the Pagoda Formation limestones in the whole Yangtze region. Till now, however, there have been different views on its origin and sedimentary environment implication. In the Western Hunan Hubei area, the limestones with the polygonal reticulate structure are mainly composed of wackestone bearing skeletal fragments of thin shelled organisms, such as ostracods, trilobites, gastropods, cephalopods and brachiopods, whereas the nets, embedded within the limestones but with no well defined boundaries, consist of clayey lime mudstone, especially rich in silt sized fragments of ostracods. Based on the studies of petrology and paleontology, this reticulate structure could not be interpreted as previously assumed, as dry cracks formed in an exposed environment, or shrinkage cracks formed on the sea bottom, or organic traces. In our opinoin, this structure is a kind of penecontemporaneous deformation structures. The original deposits of the reticulate limestone were a reverse density sequence composed of a thin, clay rich layer and an overlying thick bed of bioclasts and lime mud matrixes. Under loading process the clay rich layer intruded upwards into overlying carbonate bed, and the polygonal reticulate structure was finally formed through several stages, including the formation of load mold, and the formation of fire structure and sluicing structure(Fig.1). It is considered that the limestones of the Pagoda Formation with the polygonal reticulate structure were deposited in relatively deep environments of extra shelf and depression on the carbonate platform under normal wave base and over storm wave base. Therefore, the inferred water depth might be 50 to 150 meters.
出处 《地层学杂志》 CSCD 北大核心 2000年第4期307-309,共3页 Journal of Stratigraphy
基金 国家自然科学基金项目 !(No.49772 0 87)支持
关键词 网纹状构造 宝塔组 奥陶纪 灰岩 沉积环境 polygonal reticulate structure, penecontemporaneous deformation structure, Pagoda Formation, Western Hunan Hubei area, Ordovician
  • 相关文献

参考文献12

  • 1戎嘉余 陈旭.华南晚奥陶世的动物群分异及生物相、岩相分布模式[J].古生物学报,1987,26(5):507-545.
  • 2姬再良.华中、西南地区上奥陶统宝塔组的沉积环境初探.地层古生物论文集,12[M].北京:地质出版社,1985.87-96.
  • 3刘特民 陈学时.黔北宝塔灰岩“马蹄纹”的研究及其成因探讨.贵州地层古生物论文集[M].贵阳:贵州人民出版社,1983.169-174.
  • 4陈旭 丘金玉.宜昌奥陶纪的古环境变迁[J].地层学杂志,1986,10(1):1-15.
  • 5张文堂.中国的奥陶系.全国地层会议学术报告汇编[M].北京:科学出版社,1962.1-161.
  • 6Maurts Lindstrom,GFF,1991年,113卷,189页
  • 7陈均远,Palaeoworld,1991年,1卷,28页
  • 8戎嘉余,古生物学报,1987年,26卷,5期,507页
  • 9陈旭,地层学杂志,1986年,10卷,1期,1页
  • 10姬再良,地层古生物论文集.12,1985年,87页

共引文献18

同被引文献269

引证文献20

二级引证文献141

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