Reply to the comment of Schollnberger on ‘Subsidence analysis of salt tectonics-driven carbonate minibasins’ (Northern Calcareous Alps, Austria), published on Basin Research 2020; 00: 1– 23 doi:10.1111/bre.12500,Basin Research

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Reply to the comment of Schollnberger on ‘Subsidence analysis of salt tectonics-driven carbonate minibasins’ (Northern Calcareous Alps, Austria), published on Basin Research 2020; 00: 1– 23 doi:10.1111/bre.12500
Basin Research ( IF 2.8 ) Pub Date : 2021-05-27 , DOI: 10.1111/bre.12577
Philipp Strauss _{1,

2} , Pablo Granado ₁ , Josep Anton Muñoz ₁

Affiliation

The subsidence analysis study presented by Strauss et al. (Basin Research, 2020, doi: 10.1111/bre.12500) for Triassic carbonate platforms located in the eastern Northern Calcareous Alps shows that salt expulsion allowed for the growth of thick isolated depocenters (>1.5 km) at rates faster than that tectonic subsidence alone can provide. In this answer to a comment by Schollnberger (Basin Research, 2021, doi: 10.1111/bre.12549) we discuss in detail the rationale behind our subsidence model and the assessment of the initial salt thickness. Excellent biostratigraphic control as well as precise knowledge of paleo-bathymetry for most of the sedimentary record allowed to setup the subsidence model with well-defined boundary conditions.

中文翻译：

回复 Schollnberger 发表在 Basin Research 2020 上的“Subsidence analysis of salt tectonics-driven carbon minibasins”（奥地利北部钙质阿尔卑斯山）的评论；00: 1– 23 doi:10.1111/bre.12500

Strauss 等人提出的沉降分析研究。(Basin Research, 2020, doi: 10.1111/bre.12500) 位于北钙质阿尔卑斯山脉东部的三叠纪碳酸盐平台表明，排盐使厚的孤立沉积中心（>1.5 公里）以比单独的构造沉降更快的速度增长可以提供。在 Schollnberger（盆地研究，2021，doi：10.1111/bre.12549）的评论中，我们详细讨论了我们的沉降模型背后的基本原理和初始盐层厚度的评估。出色的生物地层控制以及对大部分沉积记录的古水深测量的精确知识允许建立具有明确边界条件的沉降模型。

更新日期：2021-05-27

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