Oligocene-Neogene lithospheric-scale reactivation of Mesozoic terrane accretionary structures in the Alaska Range suture zone, southern Alaska, USA: Reply

Trevor S. Waldien; Sarah M. Roeske; Jeffrey A. Benowitz; Evan Twelker; Meghan S. Miller

doi:10.1130/B36203.1

Oligocene-Neogene lithospheric-scale reactivation of Mesozoic terrane accretionary structures in the Alaska Range suture zone, southern Alaska, USA: Reply

Trevor S. Waldien^*, Sarah M. Roeske, Jeffrey A. Benowitz, Evan Twelker, Meghan S. Miller

^*Corresponding author for this work

Geophysics

Research output: Contribution to journal › Article › peer-review

Abstract

Topics of discussion raised by Lowey (2021) include the correlation of ultramafic-intermediate intrusions hosted within the Clearwater metasediments/ Dezadeash Formation and their displacement by the Denali fault. These topics were not main points of Waldien et al. (2021), but instead logical extrapolations of the information presented and synthesized therein. Here we re-emphasize the key findings of Waldien et al. (2021) and discuss only the relevant aspects of the ultramaficintermediate intrusions and their displacement.

Original language	English
Pages (from-to)	1083-1084
Number of pages	2
Journal	Bulletin of the Geological Society of America
Volume	134
Issue number	3-4
DOIs	https://doi.org/10.1130/B36203.1
Publication status	Published - Mar 2022

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title = "Oligocene-Neogene lithospheric-scale reactivation of Mesozoic terrane accretionary structures in the Alaska Range suture zone, southern Alaska, USA: Reply",

abstract = "Topics of discussion raised by Lowey (2021) include the correlation of ultramafic-intermediate intrusions hosted within the Clearwater metasediments/ Dezadeash Formation and their displacement by the Denali fault. These topics were not main points of Waldien et al. (2021), but instead logical extrapolations of the information presented and synthesized therein. Here we re-emphasize the key findings of Waldien et al. (2021) and discuss only the relevant aspects of the ultramaficintermediate intrusions and their displacement.",

author = "Waldien, {Trevor S.} and Roeske, {Sarah M.} and Benowitz, {Jeffrey A.} and Evan Twelker and Miller, {Meghan S.}",

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Oligocene-Neogene lithospheric-scale reactivation of Mesozoic terrane accretionary structures in the Alaska Range suture zone, southern Alaska, USA: Reply. / Waldien, Trevor S.; Roeske, Sarah M.; Benowitz, Jeffrey A. et al.
In: Bulletin of the Geological Society of America, Vol. 134, No. 3-4, 03.2022, p. 1083-1084.

Research output: Contribution to journal › Article › peer-review

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AU - Roeske, Sarah M.

AU - Benowitz, Jeffrey A.

AU - Twelker, Evan

AU - Miller, Meghan S.

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AB - Topics of discussion raised by Lowey (2021) include the correlation of ultramafic-intermediate intrusions hosted within the Clearwater metasediments/ Dezadeash Formation and their displacement by the Denali fault. These topics were not main points of Waldien et al. (2021), but instead logical extrapolations of the information presented and synthesized therein. Here we re-emphasize the key findings of Waldien et al. (2021) and discuss only the relevant aspects of the ultramaficintermediate intrusions and their displacement.

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JF - Bulletin of the Geological Society of America

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Oligocene-Neogene lithospheric-scale reactivation of Mesozoic terrane accretionary structures in the Alaska Range suture zone, southern Alaska, USA: Reply

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