<--- Back to Details
First PageDocument Content
Ultramafic rocks / Volcanology / Volcanic rocks / Peridotite / Olivine / Basalt / Tholeiitic magma series / Fractional crystallization / Igneous rock / Petrology / Geology / Igneous petrology
Date: 2007-05-21 10:23:58
Ultramafic rocks
Volcanology
Volcanic rocks
Peridotite
Olivine
Basalt
Tholeiitic magma series
Fractional crystallization
Igneous rock
Petrology
Geology
Igneous petrology

Deep Sea Drilling Project Initial Reports Volume 45

Add to Reading List

Source URL: www.deepseadrilling.org

Download Document from Source Website

File Size: 1,23 MB

Share Document on Facebook

Similar Documents

letters to nature serpentinized peridotite (Fig. 2c). Assuming a lower-crustal velocity of 3.6 km s21, the estimated maximum S-velocity perturbation of 10% near the wedge corner could represent a level of serpentinizatio

letters to nature serpentinized peridotite (Fig. 2c). Assuming a lower-crustal velocity of 3.6 km s21, the estimated maximum S-velocity perturbation of 10% near the wedge corner could represent a level of serpentinizatio

DocID: 1ro4c - View Document

Hollings IAGS talk sm.ppt

Hollings IAGS talk sm.ppt

DocID: 1rgU7 - View Document

KIMBERLITES  Kimberlite is an ultrabasic olivine-rich igneous rock called peridotite. Peridotites occur at great depths in the earth in a layer called the mantlemiles below the surface). At this depth the combi

KIMBERLITES Kimberlite is an ultrabasic olivine-rich igneous rock called peridotite. Peridotites occur at great depths in the earth in a layer called the mantlemiles below the surface). At this depth the combi

DocID: 1reER - View Document

Seismic evidence for orthopyroxene enrichment in the continental lithosphere Lara S. Wagner1, Megan L. Anderson2, Jennifer M. Jackson3, Susan L. Beck4, George Zandt4 1  Department of Geological Sciences, University of No

Seismic evidence for orthopyroxene enrichment in the continental lithosphere Lara S. Wagner1, Megan L. Anderson2, Jennifer M. Jackson3, Susan L. Beck4, George Zandt4 1 Department of Geological Sciences, University of No

DocID: 1qCXC - View Document

ARTICLE Received 29 Nov 2014 | Accepted 22 Sep 2015 | Published 3 Nov 2015 DOI: ncomms9702  OPEN

ARTICLE Received 29 Nov 2014 | Accepted 22 Sep 2015 | Published 3 Nov 2015 DOI: ncomms9702 OPEN

DocID: 1pXAr - View Document