| dc.creator |
Firstova, Anna |
|
| dc.creator |
Stepanova, Tamara |
|
| dc.creator |
Cherkashov, Georgy |
|
| dc.creator |
Goncharov, Alexey |
|
| dc.creator |
Babaeva, Svetlana |
|
| dc.date |
2016-05-12T17:00:33Z |
|
| dc.date |
2016-05-12T17:00:33Z |
|
| dc.date |
2016-03 |
|
| dc.date.accessioned |
2019-03-31T11:39:20Z |
|
| dc.date.available |
2019-03-31T11:39:20Z |
|
| dc.identifier |
Minerals 2016, 6, 19; doi:10.3390/min601001 |
|
| dc.identifier |
http://hdl.handle.net/11701/2263 |
|
| dc.identifier.uri |
https://repository.geologyscience.ru/handle/123456789/1878 |
|
| dc.description |
This paper presents mineralogical and geochemical data on seafloor massive sulfides (SMS)
from the Ashadze-1 hydrothermal field at the Mid-Atlantic Ridge (MAR). The Ashadze-1 deposit is
associated with the uplifted lower crust and upper mantle (oceanic core complex, OCC) of the MAR
segment characterized by asymmetric mode of accretion. The OCC is represented by deep-seated
gabbro-peridotite rocks exhumed on the rift valley slope along the detachment fault, during seafloor
spreading. Hydrothermal processes in OCC environments result in different deposit composition and
morphology compared to basalt-hosted systems. Abundant chimneys and enrichment in particular
metals, including copper, zinc, gold, cobalt and tin are typical for this type of SMS deposit. The
Ashadze-1 deposit is considered an example of a hydrothermal system in the initial stage of evolution
marked by the young age of the sulfides (<7.2 kyr). The mineralogy of Ashadze-1 reflects primary
ore-forming processes unaffected by post formation alteration. We propose a model for the primary
ore-forming hydrothermal process in an ultramafic-hosted environment on the modern seafloor. |
|
| dc.language |
en |
|
| dc.title |
Composition and Formation of Gabbro-Peridotite Hosted Seafloor Massive Sulfide Deposits from the Ashadze-1 Hydrothermal Field, Mid-Atlantic Ridge |
|
| dc.type |
Article |
|