意大利北部亚平宁地区Marnoso - arenacea前深层浊积岩体系的质量-输运复合物

G. Pini, C. Lucente, Sonia Venturi, K. Ogata
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引用次数: 3

摘要

Casaglia-Monte della Colonna是在山脉中发掘出的前深层演替中暴露得最好的“化石”质量运输复合体(MTC)之一,它代表了一个独特的机会,可以研究由(地质上)同时崩塌的增生楔形前缘、斜坡和盆地平原沉积物所产生的内部结构。内部结构的多样性和不同的MTC-基底相互作用取决于MTC基底接触的几何形状和再活化沉积物的来源。从我们对该MTC的首次研究开始的20年里,一些露头状况的改善以及方法和解释工具的进步使我们能够提供一个更新的情景,更详细地了解内部结构,更好地理解与基底的复杂相互作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Mass‐Transport Complexes of the Marnoso‐arenacea Foredeep Turbidite System (Northern Apennines, Italy)
The Casaglia-Monte della Colonna is one of the best exposed “fossil” mass-transport complex (MTC) cropping out in a foredeep succession exhumed in a mountain chain and represents a unique opportunity to study an internal architecture resulting from the (geologically) simultaneous collapses of an accretionary wedge front, slope, and basin plain deposits. The high variety of internal structures and the different MTC-substratum interactions depend on the geometry of MTC basal contact and the provenance of the remobilized sediments. In the 20 years from our first studies on this MTC, the better condition of some outcrops and the advances in methodological and interpretative tools enable us to provide an update scenario, with more details on the internal structures and a better comprehension of the complex interactions with the substratum.
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