高分辨率海洋地震对布雷斯特港(法国)研究的贡献

A. Baltzer, R. Boutin, Alexis Stépanian
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引用次数: 1

摘要

作为布雷斯特军事港口现代化的一部分,使用Seistec boomer进行了两次地球物理调查(2004年和2006年),使沉积物覆盖和基底深度得以识别。以前的调查已经通过钻孔确定了地质地层的垂直分层。THR地震剖面提供的“连续”视图使我们能够以不同的方式观察这些层序,并将它们与与海湾填充阶段相关的显著波浪结构联系起来。这种基金的全球视野使我们能够了解整个港口的地貌演变,而不仅仅是“点”视野。因此,奥尔恩的影响,而不是彭菲尔德的影响,如目前的规定所暗示的,是压倒性的。Translated版本:The study of The military Harbour of Brest先生(法国)(以法语发言):from a贡献甚高分辨率地震工具Within The framework of The modern of The military Harbour of Brest, two地震调查have been with The Seistec调查波姆(在2004年及2006年)观看to The sedimentary cover and depth of The rock的地下室。= =地理= =根据美国人口普查,这个县的总面积为,其中土地和(2.641平方公里)水。从VHR地震剖面获得的“连续”观点为这些垂直偏移提供了一种新的方法,因此也提供了一种新的解释:它们可能是与海湾的沉积填海相相关的特殊波浪构造。Such a global vision of the sea)的潜在to better理解the bottom楼geomorphologic进化of the harbour and to go beyond the punctual“view”。= =地理= =根据美国人口普查局的数据,该县的总面积为,其中土地和(1.)水。关键词:布雷斯特港;波姆地震;沉积物;Faults;“连续视图与点视图”。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Apport de la sismique marine très haute résolution à l’étude de la rade abri de Brest (France)
Dans le cadre de la modernisation du port militaire de Brest, deux reconnaissances geophysiques realisees avec le boomer Seistec (en 2004 et en 2006) ont permis de reconnaitre la couverture sedimentaire et la profondeur du socle. De precedentes investigations avaient etabli l’existence de decalages verticaux des couches geologiques grâce a des sondages. La vision "en continu" fournie par les profils sismiques THR permet d’apprehender de facon differente ces decalages, et de les associer a des structures ondulees remarquables, relatives a une phase de remplissage de la Baie. Cette vision globale des fonds permet de comprendre l’evolution geomorphologique de la rade dans son ensemble et de depasser la vision "ponctuelle". Ainsi, l’influence de l’Aulne, et non de la Penfeld comme le laissait supposer la disposition actuelle, s’avere preponderante. Translated version: The study of the military Harbour of Brest (France): contribution from a Very High Resolution seismic tool Within the framework of the modernisation of the military harbour of Brest, two seismic surveys have been conducted with the Seistec boomer (in 2004 and 2006) to recognize the sedimentary cover and depth of the rock basement. Previous investigations, based on drill holes, have shown the occurrence of vertical offset between geological strata. The "continuous" view acquired with the VHR seismic profiles allows a new approach of these vertical offsets and thus a new interpretation: they could be special undulating structures relative to the phase of sedimentary infilling of the bay. Such a global vision of the sea bottom floor allows to better understand the geomorphologic evolution of the harbour and to go beyond the "punctual" view. Whereas the Penfeld River seemed to be the actual active river, the influence of the Aulne River appears to have been preponderant in the sedimentary dynamics of the bay. Keywords: Brest harbor; Boomer seismic; Sediments; Faults; "Continuous versus punctual view".
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