Comment on Loreto et al., 2021: “Extensional tectonics during the Tyrrhenian back-arc basin formation and a new morpho-tectonic map”

IF 2.8 2区地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY

Basin Research Pub Date : 2023-08-28 DOI:10.1111/bre.12817

Maurizio M. Torrente, Alfonsa Milia, Magdala Tesauro

引用次数: 0

Abstract

The recent article of Loreto et al. (2021) reported new stratigraphic and structural data of the Tyrrhenian backarc basin and used them to propose a new model of crustal architecture of the basin including oceanic sectors. However, we want to open a discussion on the inconsistencies between the interpreted tectonic structures, as well as the age of faults and the data observations. In particular, data analyses and interpretations of the authors do not fully support the structural and isopach maps and models presented. Furthermore, the authors have not discussed previous published data/interpretations on timing and structural style of the rifting of the region.

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对Loreto等人的评论，2021：“第勒尼安弧后盆地形成期间的伸展构造和新的形态构造图”

Loreto等人最近的一篇文章（2021）报道了第勒尼安弧后盆地的新地层和结构数据，并利用这些数据提出了包括海洋板块在内的盆地地壳结构的新模型。然而，我们想就解释的构造结构、断层年龄和数据观测之间的不一致性展开讨论。特别是，作者的数据分析和解释并不完全支持所提出的结构图和等厚图及模型。此外，作者没有讨论之前发表的关于该地区裂谷作用的时间和结构风格的数据/解释。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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来源期刊

Basin Research 地学-地球科学综合

CiteScore

7.00

自引率

9.40%

发文量

审稿时长

>12 weeks

期刊介绍： Basin Research is an international journal which aims to publish original, high impact research papers on sedimentary basin systems. We view integrated, interdisciplinary research as being essential for the advancement of the subject area; therefore, we do not seek manuscripts focused purely on sedimentology, structural geology, or geophysics that have a natural home in specialist journals. Rather, we seek manuscripts that treat sedimentary basins as multi-component systems that require a multi-faceted approach to advance our understanding of their development. During deposition and subsidence we are concerned with large-scale geodynamic processes, heat flow, fluid flow, strain distribution, seismic and sequence stratigraphy, modelling, burial and inversion histories. In addition, we view the development of the source area, in terms of drainage networks, climate, erosion, denudation and sediment routing systems as vital to sedimentary basin systems. The underpinning requirement is that a contribution should be of interest to earth scientists of more than one discipline.