2008Science and Technology of West ChinaRequires access

Structural Feafure and Its Evolution in Gaobei Coal Mine of Longyong Coal-field

Yinxing Li

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Abstract

The paper is anglysed the mine structural evolution process through the feature of Gaobei area.The Gaobei Syncline is major fold,formed a lot of secondary folds later period.Exists three type of decollement fault,reversed fault and little fault.Tectonic revolution is following:decollement faut was formed in latter period of Indo-China.Gaobei Syncline in early period of Yanshan;mine rim fault in middle period of Yanshan.and Comolexed the principal fold.

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The paper is anglysed the mine structural evolution process through the feature of Gaobei area.The Gaobei Syncline is major fold,formed a lot of secondary folds later period.Exists three type of decollement fault,reversed fault and little fault.Tectonic revolution is following:decollement faut was formed in latter period of Indo-China.Gaobei Syncline in early period of Yanshan;mine rim fault in middle period of Yanshan.and Comolexed the principal fold.

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Available abstract

The paper is anglysed the mine structural evolution process through the feature of Gaobei area.The Gaobei Syncline is major fold,formed a lot of secondary folds later period.Exists three type of decollement fault,reversed fault and little fault.Tectonic revolution is following:decollement faut was formed in latter period of Indo-China.Gaobei Syncline in early period of Yanshan;mine rim fault in middle period of Yanshan.and Comolexed the principal fold.

Key concepts: Syncline, Décollement, Geology, Coal, Fold (higher-order function), Mining engineering, Fault (geology), Period (music)

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