Physiocochemical study of skarn formation in the Shinyama iron- copper ore deposit of the Kamaishi mine, northeastern Japan.

E. Uchida; J. T. Iiyama

doi:10.2113/gsecongeo.77.4.809

Physiocochemical study of skarn formation in the Shinyama iron- copper ore deposit of the Kamaishi mine, northeastern Japan.

E. Uchida, J. T. Iiyama

Research output: Contribution to journal › Article › peer-review

7 Citations (Scopus)

Abstract

This typical Japanese Fe-Cu skarn deposit is zoned from limestone, clinopyroxene skarn, garnet, skarn, garnet- clinopyroxene skarn, epidote-clinopyroxene skarn, epidote-amphibole skarn, plagioclase-amphibole skarn, and diorite to diorite porphyry. The 4D Cu orebody is in the clinopyroxene skarn and the 7D Fe-Cu orebody is located between garnet and garnet-clinopyroxene skarns. -K.A.R.

Original language	English
Pages (from-to)	809-822
Number of pages	14
Journal	Unknown Journal
Volume	77
Issue number	4
DOIs	https://doi.org/10.2113/gsecongeo.77.4.809
Publication status	Published - 1982 Jan 1
Externally published	Yes

ASJC Scopus subject areas

Geophysics
Geology
Geochemistry and Petrology
Economic Geology

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title = "Physiocochemical study of skarn formation in the Shinyama iron- copper ore deposit of the Kamaishi mine, northeastern Japan.",

abstract = "This typical Japanese Fe-Cu skarn deposit is zoned from limestone, clinopyroxene skarn, garnet, skarn, garnet- clinopyroxene skarn, epidote-clinopyroxene skarn, epidote-amphibole skarn, plagioclase-amphibole skarn, and diorite to diorite porphyry. The 4D Cu orebody is in the clinopyroxene skarn and the 7D Fe-Cu orebody is located between garnet and garnet-clinopyroxene skarns. -K.A.R.",

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Y1 - 1982/1/1

N2 - This typical Japanese Fe-Cu skarn deposit is zoned from limestone, clinopyroxene skarn, garnet, skarn, garnet- clinopyroxene skarn, epidote-clinopyroxene skarn, epidote-amphibole skarn, plagioclase-amphibole skarn, and diorite to diorite porphyry. The 4D Cu orebody is in the clinopyroxene skarn and the 7D Fe-Cu orebody is located between garnet and garnet-clinopyroxene skarns. -K.A.R.

AB - This typical Japanese Fe-Cu skarn deposit is zoned from limestone, clinopyroxene skarn, garnet, skarn, garnet- clinopyroxene skarn, epidote-clinopyroxene skarn, epidote-amphibole skarn, plagioclase-amphibole skarn, and diorite to diorite porphyry. The 4D Cu orebody is in the clinopyroxene skarn and the 7D Fe-Cu orebody is located between garnet and garnet-clinopyroxene skarns. -K.A.R.

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Physiocochemical study of skarn formation in the Shinyama iron- copper ore deposit of the Kamaishi mine, northeastern Japan.

Abstract

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