碳酸盐岩平台元素沉积序列发展中的适应与碳酸盐岩生产关系:下普罗旺斯西部泰索-贝里亚时代序列

Hélène Dalmasso, Marc Floquet
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引用次数: 9

摘要

下普罗旺斯西部碳酸盐岩台地(法国东南部)的提通尼亚—贝里亚系列是由非常高频的米制尺度的基本沉积层序叠加而成,一般呈上浅状,频繁出现出盖。通过对该序列的研究,可以更好地了解这些序列的控制因素。根据层序厚度建立的Fischer图和根据古深度数据建立的类似图表明,正向调节的变化并不完全控制这些层序的发育。浅海碳酸盐生产和/或聚集的变化具有相当重要的意义,因为它们直接改变了正调节/沉积供应的比例。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Relation accommodation–production carbonatée dans le développement de séquences de dépôt élémentaires de plate-forme carbonatée : la série d'âge Tithonien–Berriasien de basse Provence occidentale

The Tithonian–Berriasian series of the western Basse Provence carbonate platform (southeast France) is made of the stacking of very high frequency elementary depositional sequences, of metric scale, generally shallowing upward and frequently with emergent caps. The study of this series brings a better understanding of the controlling factors of these sequences. Fischer plots built from the sequence thicknesses and analogous diagrams built from the palaeodepths data suggest that the variations of positive accommodation do not exclusively control the development of these sequences. Variations of neritic carbonate production and/or accumulation have a considerable importance as far as they directly modify the ratio positive accommodation/sedimentary supplies.

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