含油气盆地蒸发盐矿物成因类型及其地质意义*
, 李长志Genesis of evaporites in petroliferous basins and the sedimentary and climatic significances
Guo Pei1, 2 , Li Chang-Zhi2
, Li Chang-Zhi
含油气盆地蒸发盐矿物成因类型及其地质意义* |
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郭佩, 李长志 |
Genesis of evaporites in petroliferous basins and the sedimentary and climatic significances |
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Guo Pei
, Li Chang-Zhi |
| 准噶尔盆地上古生界风城组硅硼钠石产状 A,B—岩心和薄片中断续层状、团块状硅硼钠石,非原始沉积,风南1井,4238.66 m( Guo et al ., 2021a );C,D—硅硼钠石交代碳钠镁石和碳钠钙石,硅硼钠石晶体表面可见碳钠镁石、碳钠钙石的交代残余结构,风南3井,4129.6 m,正交偏光;E—云质泥岩中的自形状硅钠石,自生成岩或交代成岩成因,风南3井,4129.6 m,正交偏光;F—纹层状泥岩中的蝴蝶状硅硼钠石,刺穿原始矿物纹层,自生成岩成因,风南1井,4338.33 m,单偏光( Guo et al ., 2021a ) |
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