Constraints on the age of formation of seismically reflective middle and lower crust beneath the Bering Shelf: SHRIMP zircon dating of xenoliths from Saint Lawrence Island

Seismic reflection and/or refraction studies reveal reflective middle and lower crust and a sharp Moho (∼32 km depth) beneath a broad region of the Bering Shelf between Alaska and northeast Russia. Basalt flows on Saint Lawrence Island of the late Cenoz

Bibliographic Details
Main Authors: Miller, Elizabeth L., Klemperer, Simon, Wirth, K, Akinin, Vyacheslav, Brocher, Thomas M, Ireland, Trevor
Format: Book Part
Language:unknown
Published: Geological Society of America Inc
Subjects:
Lawrence Island
Bering Shelf
Arctic
Alaska
Online Access:http://hdl.handle.net/1885/92339
https://doi.org/10.1130/0-8137-2360-4.195
https://openresearch-repository.anu.edu.au/bitstream/1885/92339/5/MigratedxPub23404_RSD_2002.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/92339/7/01_Miller_Constraints_on_the_age_of_2002.pdf.jpg
Description
Summary:Seismic reflection and/or refraction studies reveal reflective middle and lower crust and a sharp Moho (∼32 km depth) beneath a broad region of the Bering Shelf between Alaska and northeast Russia. Basalt flows on Saint Lawrence Island of the late Cenoz

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