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

Etsuo Uchida, J. T. Iiyama

Research output: Contribution to journalArticle

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 languageEnglish
Pages (from-to)809-822
Number of pages14
JournalEconomic Geology
Volume77
Issue number4
DOIs
Publication statusPublished - 1982
Externally publishedYes

Fingerprint

Ore deposits
skarn
Garnets
ore deposit
garnets
Copper
Japan
Iron
Amphibole Asbestos
deposits
minerals
copper
diorite
iron
clinopyroxene
amphiboles
garnet
Calcium Carbonate
limestone
epidote

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics
  • Engineering(all)

Cite this

Physiocochemical study of skarn formation in the Shinyama iron- copper ore deposit of the Kamaishi mine, northeastern Japan. / Uchida, Etsuo; Iiyama, J. T.

In: Economic Geology, Vol. 77, No. 4, 1982, p. 809-822.

Research output: Contribution to journalArticle

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