Deep-sea record of impact apparently unrelated to mass extinction in the Late Triassic

The 34-million-year (My) interval of the Late Triassic is marked by the formation of several large impact structures on Earth. Late Triassic impact events have been considered a factor in biotic extinction events in the Late Triassic (e.g., end-Triassic extinction event), but this scenario remains c...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Prif Awduron: Onoue, Tetsuji, Sato, Honami, Nakamura, Tomoki, Noguchi, Takaaki, Hidaka, Yoshihiro, Shirai, Naoki, Ebihara, Mitsuru, Osawa, Takahito, Hatsukawa, Yuichi, Toh, Yosuke, Koizumi, Mitsuo, Harada, Hideo, Orchard, Michael J., Nedachi, Munetomo
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: National Academy of Sciences 2012
Pynciau:
Physical Sciences
Mynediad Ar-lein:https://ncbi.nlm.nih.gov/pmc/articles/PMC3511106/
https://ncbi.nlm.nih.gov/pubmed/23129649
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1209486109
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