<--- Back to Details
First PageDocument Content
Geology / Petrology / Ultramafic rocks / Silicate minerals / Kimberlite / Peridotite / Harzburgite / Phlogopite / Enstatite / Xenolith / Olivine / Basalt
Date: 2016-04-04 14:15:46
Geology
Petrology
Ultramafic rocks
Silicate minerals
Kimberlite
Peridotite
Harzburgite
Phlogopite
Enstatite
Xenolith
Olivine
Basalt

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

Add to Reading List

Source URL: www.uky.edu

Download Document from Source Website

File Size: 1,25 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