The geological-event reference system, a step towards geological data harmonization

B. Le Bayon, M. Padel, T. Baudin, F. Cagnard, B. Issautier, H. Tissoux, Caroline Prognon, A. Plunder, S. Grataloup, F. Lacquement, A. Hertout, Juliette Stephan-Perrey
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Abstract

The temporal dimension is an inherent component of geology. In this regard, traditional geological maps can represent a few geological events, yet they hardly account for the entire complex rock history whether sedimentary, crystalline or volcanic. Here, using the RGF research program (French Geological Reference platform) we propose a new methodology based on digital technology and the French historical collection of 50 000-scale geological maps. This innovative approach consists of describing, organizing and hierarchizing a series of geological events within a reference framework and linking it to GIS map geometries (polygons, faults, points). In this way, the complete history of geological features can be compiled and stored in digital maps, combining distinct geological events and properties. For a single event, all associated transformations can be represented on maps, facilitating the production of real “palaeo-geological" maps that consider not only traditional sedimentary environments but also possible synchronous weathering, metamorphism, and volcanism. We discuss here an example of French Pyrenees orogenic history. The approach demonstrated here on geological maps can be used with other geological data media (boreholes, seismic reflection profiles, etc.) and thus facilitate a 3-to-4D scale, with a significant ability to address not only academic community needs, but also themes or issues related to applications required by politics, civil engineering, and society itself, to confront challenges such as natural and anthropic risk reduction and subsurface uses.
地质事件参考系统,迈向地质数据协调的一步
时间维度是地质学的一个固有组成部分。在这方面,传统的地质图可以代表一些地质事件,但它们很难解释整个复杂的岩石历史,无论是沉积的、结晶的还是火山的。在这里,我们利用RGF研究项目(法国地质参考平台)提出了一种基于数字技术和法国50000比例尺地质地图历史收藏的新方法。这种创新的方法包括在参考框架内描述、组织和分层一系列地质事件,并将其与GIS地图几何(多边形、断层、点)联系起来。通过这种方式,地质特征的完整历史可以汇编并存储在数字地图中,结合不同的地质事件和性质。对于一个单一的事件,所有相关的变化都可以在地图上表示出来,这有助于制作真正的“古地质”地图,不仅考虑传统的沉积环境,还考虑可能的同步风化、变质和火山作用。我们在此讨论法国比利牛斯山脉造山史的一个例子。这里在地质图上展示的方法可以与其他地质数据介质(钻孔、地震反射剖面等)一起使用,从而促进3到4维尺度,不仅具有解决学术界需求的显著能力,而且还具有解决与政治、土木工程和社会本身所需的应用相关的主题或问题的能力,以应对诸如自然和人为风险降低以及地下利用等挑战。
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