| Locality type: | Hydrothermal Vent |
| Classification |
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| Species: | 'Chlorite Group' (not an IMA approved species) |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Chlorite Group data |
| Locality Data: | Click here to view Roman Ruin vent, PACMANUS hydrothermal field, Manus Basin, Bismarck Sea, Papua New Guinea |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 900529 |
| Long-form Identifier: | 1:3:900529:7 |
| GUID (UUID V4): | eb51a21a-8e4d-4996-8533-ea921962a4c7 |
| Nearest other occurrences of Chlorite Group |
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|
| 3.6km (2.3 miles) | ⓘPACMANUS hydrothermal field, Manus Basin, Bismarck Sea, Papua New Guinea |
| References |
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Vanko, D. A., Bach, W., Roberts, S., Yeats, C. J., & Scott, S. D. (2004). Fluid inclusion evidence for subsurface phase separation and variable fluid mixing regimes beneath the deep‐sea PACMANUS hydrothermal field, Manus Basin back arc rift, Papua New Guinea. Journal of Geophysical Research: Solid Earth, 109(B3). |
