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首页> 外文期刊>AAPG Bulletin >Architecture, growth patterns, and early diagenetic modifications of a greenhouse ramp to rimmed shelf system: Danian of the Urbasa-Andia plateau, western Pyrenees, North Spain
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Architecture, growth patterns, and early diagenetic modifications of a greenhouse ramp to rimmed shelf system: Danian of the Urbasa-Andia plateau, western Pyrenees, North Spain

机译:温室坡道到边缘陆架系统的建筑、生长模式和早期成岩改造:西班牙北部比利牛斯山脉西部乌尔巴萨-安迪亚高原的达尼安

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摘要

The Danian carbonates exposed in the Urbasa-Andia plateau (western Pyrenees, North Spain) provide the opportunity to examine at different scales the facies types and architecture of a greenhouse ramp to rimmed shelf from the slope to coralgal reefal margin through to the highly restricted evaporitic inner shelf areas, integrated with a range of porosity-forming, early diagenetic phases associated with third-order highstands and lowstands. The detailed nature of the stratal architecture of this greenhouse system provides an understanding of potential reservoir layering, lateral facies and facies cycle changes, and widespread early dolomitization but significantly allows a whole paleokarst macroporosity systemrelated to a third-order lowstand to be accessed, illustrating how eogenetic karstic porosity can vary drastically from margins to shelf interiors. The outcrops serve as potential analogs for fields in Paleocene carbonates in North Africa and the Middle East and also offer valuable depositional and digenetic models for greenhouse platforms of other ages.
机译:暴露在乌尔巴萨-安迪亚高原(西班牙北部比利牛斯山脉西部)的达尼亚碳酸盐岩提供了在不同尺度上检查从斜坡到珊瑚礁边缘到高度受限的蒸发内架区域的温室斜坡到边缘大陆架的相类型和结构的机会,与一系列与三级高位和低位相关的孔隙形成的早期成岩相相结合。该温室系统地层结构的详细性质提供了对潜在储层层、侧相和相循环变化以及广泛的早期白云石化的理解,但显着允许进入与三级低地相关的整个古奥卡斯特大孔隙系统,说明从边缘到陆架内部的岩溶孔隙度如何发生巨大变化。这些露头是北非和中东古新世碳酸盐岩田的潜在类似物,也为其他年龄的温室平台提供了有价值的沉积和双成因模型。

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