罗马尼亚东北潘诺尼亚盆地与西北特兰西瓦尼亚盆地交界的中新世构造活动:新地震资料的启示

IF 2.2 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY Terra Nova Pub Date : 2023-08-18 DOI:10.1111/ter.12677
I. Panea, I. Munteanu, C. Gaina, V. Mocanu, R. Roban, Catalin-Florin Bouaru
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引用次数: 0

摘要

Baia Mare地区(罗马尼亚)位于东喀尔巴阡山脉、潘诺尼亚盆地和特兰西瓦尼亚盆地的交界处,有着复杂的地质历史,见证了三个主要构造省之间的相互作用。在这里,我们报告了新的地震反射测量结果,这些结果提供了有关地下地质结构的现代信息。对研究区新获得的和老式地震反射数据的综合分析揭示了潘诺尼亚东北部和特兰西瓦尼亚西北部盆地接触处古近系和新近系矿床的结构细节。特别是,它揭示了一个断层带,该断层带很可能控制了东潘诺尼亚和特兰西瓦尼亚盆地的构造演化。更好地了解研究区的地壳结构和构造特征是评估该地区地热潜力的第一步。
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Miocene tectonic activity at the boundary between NE Pannonian and NW Transylvanian basins (Romania): Insight from new seismic data
Situated at the junction between the Eastern Carpathians Mountains, the Pannonian and the Transylvanian basins, the Baia Mare region (Romania) has a complex geological history that witnessed the interaction among the three main tectonic provinces. Here, we report results from new seismic reflection measurements that provide modern information about the subsurface geological structure. The integrated analysis of the newly acquired and vintage seismic reflection data from the study area reveals details about the architecture of the Palaeogene and the Neogene deposits at the contact between the northeastern Pannonian and northwestern Transylvanian basins. In particular, it unveils a fault zone that most probably controlled the tectonic evolution of the eastern Pannonian and Transylvanian basins. A better understanding of the crustal structure and tectonic features in the study area is a first step into evaluating the geothermal potential of the region.
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来源期刊
Terra Nova
Terra Nova 地学-地球科学综合
CiteScore
4.80
自引率
8.30%
发文量
59
审稿时长
2.3 months
期刊介绍: Terra Nova publishes short, innovative and provocative papers of interest to a wide readership and covering the broadest spectrum of the Solid Earth and Planetary Sciences. Terra Nova encompasses geology, geophysics and geochemistry, and extends to the fluid envelopes (atmosphere, ocean, environment) whenever coupling with the Solid Earth is involved.
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