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 |
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Pages (from-to) | 809-822 |
Number of pages | 14 |
Journal | Unknown Journal |
Volume | 77 |
Issue number | 4 |
DOIs | |
Publication status | Published - 1982 Jan 1 |
Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Geology
- Geochemistry and Petrology
- Economic Geology