Origin of Cu in the PACMANUS hydrothermal field from the eastern Manus back-arc basin: evidence from mass balance modeling
Author:
Publisher
Springer Science and Business Media LLC
Subject
Aquatic Science,Oceanography
Link
http://link.springer.com/content/pdf/10.1007/s13131-019-1475-z.pdf
Reference81 articles.
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2. Auzende J M, Urabe T. 1996a. Cruise explores hydrothermal vents of the Manus Basin. Eos, Transactions American Geophysical Union, 77: 244, doi: 10.1029/96EO00174
3. Auzende J M, Urabe T. 1996b. Submersible observation of tectonic, magmatic and hydrothermal activity in the Manus Basin (Papua New Guinea). Eos, Transactions American Geophysical Union, 77: 115
4. Ballhaus C, Ryan C G, Mernagh T P, et al. 1994. The partitioning of Fe, Ni, Cu, Pt, and Au between sulfide, metal, and fluid phases: a pilot study. Geochimica et Cosmochimica Acta, 58(2): 811–826, doi: 10.1016/0016-7037(94)90507-X
5. Bartetzko A, Paulick H, Iturrino G, et al. 2003. Facies reconstruction of a hydrothermally altered dacite extrusive sequence: evidence from geophysical downhole logging data (ODP Leg 193). Geochemistry, Geophysics, Geosystems, 4(10): 1087
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