Thermal history of lithosphere formed beneath fast spreading ridges: Constraints from the Mantle Transition Zone of the East Pacific Rise at Hess Deep and Oman Drilling Project, Wadi Zeeb, Samail ophiolite

2021 ◽  
Author(s):  
Nadine L. Grambling ◽  
Nicholas Dygert ◽  
Beau Boring ◽  
Marlon M. Jean ◽  
Peter B. Kelemen
Keyword(s):  
Transition Zone ◽  
Thermal History ◽  
East Pacific Rise ◽  
Mantle Transition Zone ◽  
East Pacific ◽  
Spreading Ridges ◽  
Fast Spreading ◽  
History Of ◽  
Drilling Project

scholarly journals Crustal Magmatic System Beneath the East Pacific Rise (8°20′ to 10°10′N): Implications for Tectonomagmatic Segmentation and Crustal Melt Transport at Fast‐Spreading Ridges

2018 ◽  
Vol 19 (11) ◽  
pp. 4584-4611 ◽  
Author(s):  
Milena Marjanović ◽  
Suzanne M. Carbotte ◽  
Hélène D. Carton ◽  
Mladen R. Nedimović ◽  
Juan Pablo Canales ◽  
...  
Keyword(s):  
East Pacific Rise ◽  
Magmatic System ◽  
East Pacific ◽  
Spreading Ridges ◽  
Fast Spreading ◽  
Melt Transport

scholarly journals Is the Lower Crust Convecting Beneath Mid-Ocean Ridges?

Eos ◽  
2017 ◽  
Author(s):  
Terri Cook
Keyword(s):  
Hydrothermal Vent ◽  
Lower Crust ◽  
East Pacific Rise ◽  
Hydrothermal Circulation ◽  
Ocean Ridges ◽  
East Pacific ◽  
Spreading Ridges ◽  
Fast Spreading ◽  
Couple Models

The first attempt to couple models of hydrothermal circulation and magmatic convection along fast-spreading ridges may explain the spacing of hydrothermal vent fields along the East Pacific Rise.

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