globalchange  > 气候变化与战略
DOI: 10.1016/j.epsl.2020.116557
论文题名:
Reply to Comment on Resentini et al., 2020: “Ongoing exhumation of the Taiwan orogenic wedge revealed by detrital apatite thermochronology: The impact of effective mineral fertility and zero-track grains”
作者: Resentini A.; Malusà M.G.; Garzanti E.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2020
卷: 550
语种: 英语
中文关键词: apatite fission tracks ; detrital thermochronology ; Taiwan orogen
英文关键词: Phosphate minerals ; Fission track ; Orogenic wedge ; Thermochronology ; Fission reactions
英文摘要: In their Comment to Resentini et al. (2020), Mesalles et al. pointed out supposed fundamental inaccuracies concerning analytical aspects and the tectonic interpretation of fission-track data. This would invalidate the main conclusions of our study. Here we demonstrate that their criticism is ill-founded. © 2020 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/165230
Appears in Collections:气候变化与战略

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作者单位: Laboratory for Provenance Studies, Department of Earth and Environmental Sciences, University of Milano-Bicocca, Milano, 20126, Italy

Recommended Citation:
Resentini A.,Malusà M.G.,Garzanti E.. Reply to Comment on Resentini et al., 2020: “Ongoing exhumation of the Taiwan orogenic wedge revealed by detrital apatite thermochronology: The impact of effective mineral fertility and zero-track grains”[J]. Earth and Planetary Science Letters,2020-01-01,550
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