The latest Cretaceous‐Early Paleogene rapid growth of accretionary complex and exhumation of high pressure series metamorphic rocks in northwestern Pacific …
G Kimura - Journal of Geophysical Research: Solid Earth, 1994 - Wiley Online Library
Episodic growth of accretionary complexes along the northwestern Pacific margin is well
documented from detailed biostratigraphy and radiometric dating of metamorphic rocks. The
latest Cretaceous to early Paleogene rapid growth of the accretionary complexes observed
in Hokkaido and Sakhalin Islands was caused by the supply of a large amount of
terrigenous sediments from an intracontinent collision zone: the Mongolia‐Okhotsk zone in
the northern Asian continent. Rapid growth of the accretionary prism resulted in episodic …
documented from detailed biostratigraphy and radiometric dating of metamorphic rocks. The
latest Cretaceous to early Paleogene rapid growth of the accretionary complexes observed
in Hokkaido and Sakhalin Islands was caused by the supply of a large amount of
terrigenous sediments from an intracontinent collision zone: the Mongolia‐Okhotsk zone in
the northern Asian continent. Rapid growth of the accretionary prism resulted in episodic …
The latest Cretaceous-early Paleogene rapid growth of accretionary complex and exhumation of high pressure series metamorphic rocks in northwestern Pacific …
G Kimura - Oceanographic Literature Review, 1995 - infona.pl
Episodic growth of accretionary complexes along the northwestern Pacific margin is well
documented from detailed biostratigraphy and radiometric dating of metamorphic rocks. The
latest Cretaceous to early Paleogene rapid growth of the accretionary complexes observed
in Hokkaido and Sakhalin Islands was caused by the supply of a large amount of
terrigenous sediments from the Mongolia-Okhotsk collision zone. Rapid growth of the
accretionary prism resulted in episodic tectonic events in the forearc and magmatic arc …
documented from detailed biostratigraphy and radiometric dating of metamorphic rocks. The
latest Cretaceous to early Paleogene rapid growth of the accretionary complexes observed
in Hokkaido and Sakhalin Islands was caused by the supply of a large amount of
terrigenous sediments from the Mongolia-Okhotsk collision zone. Rapid growth of the
accretionary prism resulted in episodic tectonic events in the forearc and magmatic arc …