Home Multi-Country Search About Admin Login
Cenozoic
Cretaceous
Jurassic
Triassic
Permian

Search by
Select Region(s) to search
Hold Ctrl (Windows/Linux) or Command (Mac) to select multiple
Hidaka Metamorphic Gr
Click to display on map of the Ancient World at:
Hidaka Metamorphic Gr base reconstruction

Hidaka Metamorphic Gr


Period: 
Paleogene

Age Interval: 


Province: 
Hokkaido

Type Locality and Naming

Hidaka meta. Belt

Synonym:


Lithology and Thickness

The HIMB consists of high-temperature and low-pressure (HT-LP) metamorphic rocks up to granulite facies associated with abundant mafic to felsic plutonic rocks.

Metamorphic grade increases westwards and is cat by the east-dipping HIMT along the western (basal) margin, whereas the eastern low-grade parts of the complex grade into non-metamorphic accretionary sediments of the Nakanogawa Group lying to the east.

The HMB is divided into four metamorphic zones (Osanai et al. 1986, 1991, 1992; Komatsu et al. 1989, 1992, 1994): Zone I is character. ized by Ms + Chl (areenschist facies); Zone II comprises Bt + Ms; Zone IIT consists of Grt + Sill + Kf (both amphibolite facies); and Zone IV is characterized by Gat + Crd + Kf + Opx (granulite facies) with anatectites.


Lithology Pattern: 
Metavolcanics


Relationships and Distribution

Lower contact

No data.

Upper contact

Hidaka Plutonics Fm (unconformable)

Regional extent

Hidaka Metamorphic Belt. The belt defines an NNW-trending arc c. 120 km long and 10-20 km wide, with foliations generally steeply dipping towards the east except in southernmost areas with flat-Lying structures.


GeoJSON

{"type":"Feature","geometry":{"type":"MultiPolygon","coordinates":[[[[143.23,41.97],[143.01,42.13],[143.05,42.25],[142.91,42.42],[142.79,42.55],[142.74,42.69],[142.68,42.91],[142.67,43.01],[142.69,43.08],[142.71,43.09],[142.77,42.95],[142.8,42.85],[142.81,42.77],[142.84,42.67],[142.85,42.61],[142.89,42.54],[142.99,42.43],[143.1,42.35],[143.22,42.25],[143.29,42.16],[143.32,42.11],[143.3,42.06],[143.23,41.97]]]]}}

Fossils

No data.


Age 


Age Span: 

    Beginning stage: 
Danian

    Fraction up in beginning stage: 
0

    Beginning date (Ma): 
66.04

    Ending stage: 
Bartonian

    Fraction up in the ending stage: 
0

    Ending date (Ma):  
41.03

Depositional setting

The whole metamorphic sequence, together with the non-metamorphic sediments, is regarded as an arc crustal section down to 22-23 km (Komatsu et al. 1989, 1994).


Depositional pattern:  


Additional Information



Compiler:  

Hayato Ueda. 2g Hokkaido. in Moreno, T., WALLIS, S., Kojima, T. & Gibbons, W. (Eds) 2016. The Geology of Japan. Geological Society. London. 201-220.