卓木巴斯套组

时代属早泥盆世郁江期至四排期。分布于新疆东准噶尔地区。为灰黄、灰色中—厚层砂质灰岩与钙质砂岩互层,厚78米。含丰富的腕足类“Paraspirifer” spp.,Rhytistrophia beckii,Leptaenopyxis bouei,Megakozlowskiella sp.;珊瑚Thamnopora sp.,Syringaxon sp.等,局部富集呈介壳层。在乌鲁苏巴斯套南,底部为厚约1m的底砾岩,砾石成分复杂,有英安斑岩、石英斑岩、杏仁状安山岩等,大小不等,磨圆度中等,钙质及砂质胶结。与下伏塔黑尔巴斯套组呈不整合接触。

Concept & Semantic
  10

Contributor

contributed at 2011-10-11

Classification(s)

Earth System(in Chinese)Geostratigraphic stratigraphy

Detailed Description

EN_US
Name Zhuomubasite Fm
ZH_CN
Name 卓木巴斯套组
Description 时代属早泥盆世郁江期至四排期。分布于新疆东准噶尔地区。为灰黄、灰色中—厚层砂质灰岩与钙质砂岩互层,厚78米。含丰富的腕足类“Paraspirifer” spp.,Rhytistrophia beckii,Leptaenopyxis bouei,Megakozlowskiella sp.;珊瑚Thamnopora sp.,Syringaxon sp.等,局部富集呈介壳层。在乌鲁苏巴斯套南,底部为厚约1m的底砾岩,砾石成分复杂,有英安斑岩、石英斑岩、杏仁状安山岩等,大小不等,磨圆度中等,钙质及砂质胶结。与下伏塔黑尔巴斯套组呈不整合接触。

How to cite

NNU_Group (2020). 卓木巴斯套组, Concept & Semantic, OpenGMS, https://geomodeling.njnu.edu.cn/repository/concept/f5072ab7-9cd0-408f-9931-0ca982a339b8
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contributed at 2011-10-11

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