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Melnikovite from
EPR 21° N, Juan de Fuca Ridge complex, East Pacific Rise, Pacific Ocean


Locality type:Hydrothermal Vent
Classification
Species:'Melnikovite' (not an IMA approved species)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Melnikovite data
Locality Data:Click here to view EPR 21° N, Juan de Fuca Ridge complex, East Pacific Rise, Pacific Ocean
Data Identifiers
Mindat Occurrence Record ID:1239216
Long-form Identifier:1:3:1239216:2
GUID (UUID V4):248deadf-261c-464e-ae5c-41f0564c6151
References
Reference Search (possible matching items)
Book
01636083 0 geny G. Gurvich Sediments of the World Ocean Fundamental Theory of Deep-Sea Sedimentation 4V... Gurvich Metalliferous Sediments of the World Ocean Fundamental Theory of Deep-Sea Hydrothermal Sedimentation... Gurvich Metalliferous Sediments of the World Ocean Fundamental Theory of Deep-Sea Hydrothermal Sedimentation...1. Metalliferous sediments from the Southeast Pacific.7 1.1.1. Conditions of formation.7 1.1.2. Lithologic...part of the East Pacific Rise.51 1.3. Metalliferous sediments from the Juan de Fuca Ridge.61 1.4. Metalliferous
Book
4 Ridge Crest Magma Chambers: A Review of Results from Marine Seismic Experiments at the East Pacific...Pacific Rise Detrick, R.S. 7 Accommodation Zones and Transfer Faults: Integral Components of Mid-Atlantic...Mid-Atlantic Ridge Extensional Systems Karson, I.A. Rooting of the Sheeted Dike Complex in the Oman Ophiolite...to Decipher Successive Magmatic Events Reuber, 1. 21 39 55 83 B) Mantle 105 The Upward Migration...Regeneration Processes in Upper Mantle of Continental and Ocean Rift Zones Dobretsov, N.L. and Ashchepkov, I.V.
Book
consider internal communications. Within our complex industry secrecy and competition sometimes dictates...baseline designated 10 000 m E aligned N—S. The traverse line at 11 800 m N intersects the approximate centre...the surface expression of the body, which plunges east at about 30°, roughly conformable with enclosing...terrain of the Nanambu Complex. The Cahill Formation here dips at about 30° to the east. The Carpentarian...is from 20 to 90 m below the surface. The 11 800 m N traverse crosses the whole of the local Orebody stratigraphy
 
Mineral and/or Locality  
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