TY - JOUR
T1 - Physiocochemical study of skarn formation in the Shinyama iron- copper ore deposit of the Kamaishi mine, northeastern Japan.
AU - Uchida, E.
AU - Iiyama, J. T.
PY - 1982/1/1
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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U2 - 10.2113/gsecongeo.77.4.809
DO - 10.2113/gsecongeo.77.4.809
M3 - Article
AN - SCOPUS:0019923511
VL - 77
SP - 809
EP - 822
JO - Nuclear Physics A
JF - Nuclear Physics A
SN - 0375-9474
IS - 4
ER -