Clark, A. H., Kontak, D. J. (2004) Fe-Ti-P Oxide Melts Generated through Magma Mixing in the Antauta Subvolcanic Center, Peru: Implications for the Origin of Nelsonite and Iron Oxide-Dominated Hydrothermal Deposits. Economic Geology, 99 (2) 377-395 doi:10.2113/gsecongeo.99.2.377

| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | Fe-Ti-P Oxide Melts Generated through Magma Mixing in the Antauta Subvolcanic Center, Peru: Implications for the Origin of Nelsonite and Iron Oxide-Dominated Hydrothermal Deposits | ||
| Journal | Economic Geology | ||
| Authors | Clark, A. H. | Author | |
| Kontak, D. J. | Author | ||
| Year | 2004 (March 1) | Volume | 99 |
| Issue | 2 | ||
| Publisher | Society of Economic Geologists | ||
| DOI | doi:10.2113/gsecongeo.99.2.377Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 226422 | Long-form Identifier | mindat:1:5:226422:0 |
| GUID | 0 | ||
| Full Reference | Clark, A. H., Kontak, D. J. (2004) Fe-Ti-P Oxide Melts Generated through Magma Mixing in the Antauta Subvolcanic Center, Peru: Implications for the Origin of Nelsonite and Iron Oxide-Dominated Hydrothermal Deposits. Economic Geology, 99 (2) 377-395 doi:10.2113/gsecongeo.99.2.377 | ||
| Plain Text | Clark, A. H., Kontak, D. J. (2004) Fe-Ti-P Oxide Melts Generated through Magma Mixing in the Antauta Subvolcanic Center, Peru: Implications for the Origin of Nelsonite and Iron Oxide-Dominated Hydrothermal Deposits. Economic Geology, 99 (2) 377-395 doi:10.2113/gsecongeo.99.2.377 | ||
| In | (2004, March) Economic Geology Vol. 99 (2) Society of Economic Geologists | ||
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