| 黎乃煌,武文来.“探马石砾岩”的地质意义[J].地质找矿论丛,1987,(2):46-53 |
| “探马石砾岩”的地质意义 |
| THE GEOLOGICAL SENSE OF "TANMASHI CONGLOMERATE" |
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| DOI：10.6053/j.issn.1001-1412.1987.2. 005 |
| 中文关键词: 探马石砾岩 构造 棒石糜棱岩 |
| 英文关键词: |
| 基金项目: |
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| 摘要点击次数: 1787 |
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| 中文摘要: |
| 五台山西段的"探马石"砾岩,原被确认为系甘泉不整合西延部份的底砾岩.经研究认为"探马石"砾岩不是底砾岩,而是构造形成的棒石糜棱岩. |
| 英文摘要: |
| In this paper, the authers discuss the geological sense of "Tanmashi conglomerate" which was previously considered as basal conglomerate. But "Tanmashi conglomerate" and the similar rocks are formed during ductile-plastic deformation. So they should be considered as structural rocks (i.e. bar rock mylonite). And for this reason. the unconformity relationship proposed formerly should also be corrected |
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