The Origin of the Paleo‐Kuril Arc, NE Japan: Sediment Provenance Change and Its Implications for Plate Configuration in the NW Pacific Region Since the Late Cretaceous-Reference-Cited by-同舟云学术

The Origin of the Paleo‐Kuril Arc, NE Japan: Sediment Provenance Change and Its Implications for Plate Configuration in the NW Pacific Region Since the Late Cretaceous

Published:2022-12 Issue:12 Volume:41 Page:
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Harisma H.¹^ORCID,Naruse H.¹^ORCID,Asanuma H.²³,Hirata T.²

Affiliation:

1. Department of Geology and Mineralogy Faculty of Science Kyoto University Kyoto Japan

2. Geochemical Research Center The University of Tokyo Tokyo Japan

3. Atmosphere and Ocean Research Institute The University of Tokyo Chiba Japan

Funder

Ministry of Education, Culture, Sports, Science and Technology

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022TC007299

Reference125 articles.

1. 1:50.000 Geological Map of KIRITAPPU. (1966).Japan:Geological Survey of Hokkaido. Retrieved fromhttps://gbank.gsj.jp/geonavi/geonavi.php

2. Detrital zircons as tracers of sedimentary provenance: limiting conditions from statistics and numerical simulation

3. Compaction-induced inclination shallowing of the post-depositional remanent magnetization in a synthetic sediment

4. Tectonic erosion in a Pacific-type orogen: Detrital zircon response to Cretaceous tectonics in Japan

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