| “探马石砾岩”的地质意义 |
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| 引用本文： | 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. |
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| 作者姓名： | 黎乃煌 武文来 |
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| 作者单位： | 山西冶金地质研究所
(黎乃煌)，山西冶金地质研究所(武文来) |
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| 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.
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| 关 键 词： | 探马石砾岩 构造 棒石糜棱岩 |
THE GEOLOGICAL SENSE OF "TANMASHI CONGLOMERATE" |
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| Li Naihuang and Wu Wenlai.THE GEOLOGICAL SENSE OF "TANMASHI CONGLOMERATE"[J].Contributions to Geology and Mineral Resources Research,1987(2):46-53. |
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| Authors: | Li Naihuang and Wu Wenlai |
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| Institution: | Shanxi Geological Institute, MMI;Shanxi Geological Institute, MMI |
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| Abstract: | 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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