对Alessandretti和Warren关于“西冈瓦纳巴西利亚带泥盆纪至二叠纪造山后剥蚀:磷灰石裂变径迹热年代学的见解”的评论的回复,2021

IF 2.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS Journal of Geodynamics Pub Date : 2022-01-01 DOI:10.1016/j.jog.2021.101893
Ana Carolina Liberal Fonseca , Gabriella Vago Piffer , Simon Nachtergaele , Gerben Van Ranst , Johan De Grave , Tiago Amâncio Novo
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引用次数: 0

摘要

在此,我们回复Alessandretti和Warren(2021)对Fonseca等人(2020)的论文“西冈瓦纳Brasília带的泥盆纪至二叠纪造山后剥蚀:来自磷灰石裂变径迹热年代学的见解”的评论。我们的印象是,许多评论,至少在某种程度上源于对我们手稿的误解,也考虑到他们没有提出任何替代假设来解释我们在上述论文中提出的结果。因此,我们重申了我们对低温热年代学数据的解释。在泥盆纪至二叠纪期间,巴西利亚带基底受到了大量的侵蚀,可能是当时帕拉纳盆地东北部部分地区碎屑沉积物的源区。磷灰石裂变径迹数据表明,与Araçuaí等造山带相比,中新生代事件对Brasília带造山带后挖掘的影响有限。
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Reply to the comment on “Devonian to Permian post-orogenic denudation of the Brasília Belt of West Gondwana: insights from apatite fission track thermochronology” by Alessandretti and Warren, 2021

Here we reply to the comment by Alessandretti and Warren, (2021) on the paper “Devonian to Permian post-orogenic denudation of the Brasília Belt of West Gondwana: insights from apatite fission track thermochronology” by Fonseca et al. (2020). We have the impression that many of the remarks, at least to some extent stem from a misunderstanding of our manuscript, also considering that they did not propose any alternative hypothesis for interpretation of our results presented in the aforementioned paper. We, thus, reiterate our interpretations from our low-temperature thermochronology data. The basement of the Brasilia Belt was subject to a significant exhumation during the Devonian to the Permian through erosion, and was likely a source area for detrital sediments deposited in parts of the northeastern Paraná Basin at that time. Apatite fission-track data show that Meso-Cenozoic events had limited effect on post-orogenic exhumation of the Brasília Belt, in contrast to e.g. the Araçuaí Belt.

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来源期刊
Journal of Geodynamics
Journal of Geodynamics 地学-地球化学与地球物理
CiteScore
4.60
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: The Journal of Geodynamics is an international and interdisciplinary forum for the publication of results and discussions of solid earth research in geodetic, geophysical, geological and geochemical geodynamics, with special emphasis on the large scale processes involved.
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