| Locality type: | Zone |
| Classification |
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| Species: | 'Serpentine Subgroup' (not an IMA approved species) |
| Formula: | D3[Si2O5](OH)4 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Serpentine Subgroup data |
| Locality Data: | Click here to view Atlantis II Fracture Zone, Southwest Indian Ridge, Indian Ocean |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 241722 |
| Long-form Identifier: | 1:3:241722:6 |
| GUID (UUID V4): | 9fed3da3-001c-459f-a0be-57029108b458 |
| References |
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| Reference Search (possible matching items) |
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 | | Book | | chromium mine of Agios Stefanos, located a few km southwest of the Domokos village (Figure 1B). In the studied...which were eventually obducted onto the Pelagonian Zone, during the Late Jurassic-Early Cretaceous [11–14]...oceanic seamounts or to ocean-continent transition zones; ii) normal-type mid-ocean ridge (N-MORB); and iii)...erupted close to the rifted margin of an ocean-continent transition zone. Radiolarian data from interbedded...[16–18]), while the latter formed in a supra-subduction zone (SSZ) setting [17–19]. This difference is reflected |
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