Age constraint for the Moreno Hill Formation (Zuni Basin) by CA-TIMS and LA-ICP-MS detrital zircon geochronology
The “mid-Cretaceous” (~125–80 Ma) was punctuated by major plate-tectonic upheavals resulting in widespread volcanism, mountain-building, eustatic sea-level changes, and climatic shifts that together had a profound impact on terrestrial biotic assemblages. Paleontological evidence suggests terrestria...
Main Authors: | Charl D. Cilliers, Ryan T. Tucker, James L. Crowley, Lindsay E. Zanno |
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Format: | Article |
Language: | English |
Published: |
PeerJ Inc.
2021-03-01
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Series: | PeerJ |
Subjects: | |
Online Access: | https://peerj.com/articles/10948.pdf |
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