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Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China

王国芝 刘树根 马永生 徐国盛 蔡勋育

王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China[J]. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1
引用本文: 王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China[J]. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1
王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1
Citation: 王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1

Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China

doi: 10.1007/s12583-010-0093-1

Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China

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出版历程
  • 收稿日期:  2018-07-15
  • 修回日期:  2018-07-15
  • 刊出日期:  2018-07-15

Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China

doi: 10.1007/s12583-010-0093-1

摘要: Tectonic uplift at the end of Sinian resulted in the denudation of the Dengying (灯影) Formation on a different scale and the development of a great number of secondary dissolution vugs beneath the unconformity between Sinian and Cambrian. Geological and geochemical characteristics such as the development of caves, sinkholes, karst tubes and weathering crust, abrupt depletion and negative deflection of δ13C and δ18O in country rock and vug filling toward unconformity surface suggest that subaerial karstification is responsible for the development of secondary karst vugs within 150 m or so beneath the unconformity surface...

English Abstract

王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China[J]. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1
引用本文: 王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China[J]. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1
王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1
Citation: 王国芝, 刘树根, 马永生, 徐国盛, 蔡勋育. Characteristics of Subaerial Karstification and Late Reconstruction in the Dengying Formation, Sichuan Basin, Southwestern China. Journal of Earth Science, 2010, 12(3). doi: 10.1007/s12583-010-0093-1

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