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首页> 外文期刊>Near surface geophysics >An integrated geophysical study of the western part of the Rochechouart-Chassenon impact structure, Charente, France
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An integrated geophysical study of the western part of the Rochechouart-Chassenon impact structure, Charente, France

机译:法国夏朗德省Rochechouart-Chassenon撞击结构西部的综合地球物理研究

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摘要

A multi-method geophysical survey was carried out with the aim of reassessing the structure of the Rochechouart-Chassenon astrobleme and the geometry of the impact-related formations, referred to as fallout breccias, in the vicinity of Chassenon. Gravity data extracted from the BRGM InfoTerre database were reprocessed and revealed both the shape of the astrobleme and the presence of a small negative gravity anomaly close to Chassenon, due to the low density of impact-related rocks; a 2D gravity model across the fallout deposits was provided. Geological settings, well-logging and geophysical soundings (direct current (DC), time-domain electromagnetic (TDEM) and frequencydomain electromagnetic (FDEM)) were carried out on the fallout breccias at Chassenon. The ID resistivity models based on TDEM and DC soundings, resulting from a mutually constrained inversion and coupled with ID models of PDEM data, were constrained by borehole data and provided 2D resistivity models across the fallout deposits of Chassenon. The combination of these methods allows the description of both the impact-related rocks geometry and the global structure of fallout breccia remains at Chassenon. The study also shows that the fallout breccia has a complex structure, consisting of thin layers of lithic breccia and suevite, the total thickness of which is larger at Chassenon than previously estimated by means of geological analysis.
机译:进行了一次多方法的地球物理调查,目的是重新评估罗森霍亚特-沙森农天体的结构和沙森农附近的与冲击有关的地层的几何结构,即沉降角砾岩。对从BRGM InfoTerre数据库中提取的重力数据进行了重新处理,并揭示了冲击波的形状以及由于与冲击有关的岩石密度低而在Chassenon附近出现了一个小的负重力异常。提供了跨沉降沉积物的二维重力模型。在Chassenon的沉降角砾岩上进行了地质设置,测井和地球物理探测(直流(DC),时域电磁(TDEM)和频域电磁(FDEM))。基于TDEM和DC测深的ID电阻率模型,是由相互约束的反演产生的,并与PDEM数据的ID模型耦合,受到井眼数据的约束,并提供了沿Chassenon沉积物的二维电阻率模型。这些方法的组合可以描述与冲击有关的岩石的几何形状,也可以描述Chassenon沉降角砾岩的整体结构。研究还表明,沉降角砾岩具有复杂的结构,由薄层角砾岩角砾岩和苏维岩组成,在沙瑟农角的总厚度比以前通过地质分析估计的要大。

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