Geology and Metamorphism of the Itoigawa-Omi Area of the Hida Gaien Belt, Central Japan: Reconstruction of the Oldest Pacific-type High P/T Type Metamorphism and Hydration Metamorphism during Exhumation
-
- MATSUMOTO Ken-ichi
- Faculty of Human Development, University of Toyama
-
- SUGIMURA Kazuko
- Department of Earth and Planetary Science, The University of Tokyo
-
- TOKITA Izumi
- Graduate School of Education, Toyama University
-
- KUNUGIZA Keitaro
- Faculty of Human Development, University of Toyama
-
- MARUYAMA Shigenori
- Department of Earth and Planetary Sciences, Tokyo Institute of Technology
Bibliographic Information
- Other Title
-
- 飛騨外縁帯糸魚川‐青海地域の地質と変成作用―日本列島地質体最古の沈み込み帯型変成作用と上昇期の加水変成作用―
- 飛騨外縁帯糸魚川-青海地域の地質と変成作用--日本列島地質体最古の沈み込み帯型変成作用と上昇期の加水変成作用
- ヒダ ガイエンタイ イトイガワ オウミ チイキ ノ チシツ ト ヘンセイ サヨウ ニホン レットウ チシツタイ サイコ ノ シズミ コミ オビガタ ヘンセイ サヨウ ト ジョウショウキ ノ カスイ ヘンセイ サヨウ
- Geology and metamorphism of the Itogawa-Omi Area of the Hida Gaien Belt, Central Japan: reconstruction of the oldest Pacific-type high P/T type metamorphism and hydration metamorphism during exhumation
- Reconstruction of the Oldest Pacific-type High P/T Type Metamorphism and Hydration Metamorphism during Exhumation
- ―日本列島地質体最古の沈み込み帯型変成作用と上昇期の加水変成作用―
Search this article
Abstract
The geology and petrology of the Itoigawa–Omi area of the Hida Gaien belt have been reexamined with pioneering metamorphic zonal mapping of glaucophane schist facies done by Banno (1958). A geologic study shows that crystalline schists of ca. 262-381 Ma, 450 Ma garnet amphibolite, amphibolite, 520 Ma jadeitite, albitite, and rodingite, reaching 10 km long and 2-5 km wide, occur as tectonic blocks of serpentinite forming the Omi serpentinite melange (OSM).<br> Along the Omi–River of the eastern side of the OSM, chlorite, garnet, and biotite zones of pelitic schists are again recognized across several tectonic blocks of schist, indicating the slightly broken nature of a large metamorphic unit that resulted probably from exhumation of the serpentinite mélange belt. Kfs and chlorite are common throughout pelitic schists along the Omi–River. Thus, biotite- and oligclase-forming reactions may have been K-feldspar + chlorite → muscovite + biotite + quartz + H2O, and muscovite + clinozoisite + quartz → K-feldspar + anorthite + H2O, respectively. <br> Glaucophane described by Banno (1958) in the chlorite zone of the Omi River has been recognized in composite grains consisting of hornblende core, gluacophane mantle, and actinolite rim. In contrast, glaucophane appears in a few samples along with eclogitic assemblages as plurifacial minerals before, during, and after eclogite facies in the pelitic schists of the western side of OSM (EC unit). Thus, the regional metamorphism described along the Omi–river of OSM (EA unit) is not a retrogressive metamorphism of the EC unit, but a regional hydrothermal recrystallization just before or during exhumation in the serpentinite mélange belt.
Journal
-
- Journal of Geography (Chigaku Zasshi)
-
Journal of Geography (Chigaku Zasshi) 120 (1), 4-29, 2011
Tokyo Geographical Society
- Tweet
Keywords
Details 詳細情報について
-
- CRID
- 1390001204229560960
-
- NII Article ID
- 10030371645
-
- NII Book ID
- AN00322536
-
- ISSN
- 18840884
- 0022135X
- http://id.crossref.org/issn/00221341
-
- NDL BIB ID
- 11043914
-
- Text Lang
- ja
-
- Data Source
-
- JaLC
- NDL
- Crossref
- CiNii Articles
-
- Abstract License Flag
- Disallowed