<--- Back to Details
First PageDocument Content
Chemistry / Mars / Earth sciences / Igneous rocks / Magnesite / Pyroxene / Olivine / Mineral / Pyroxenite / Crystallography / Meteorite types / Matter
Date: 2000-05-08 15:41:45
Chemistry
Mars
Earth sciences
Igneous rocks
Magnesite
Pyroxene
Olivine
Mineral
Pyroxenite
Crystallography
Meteorite types
Matter

Lunar and Planetary Science XXVIII PRECIPITATION AND REACTION PRODUCTS OF FLUIDS IN MARTIAN ORTHOPYROXENITE ALH84001. G.Kurat*, M.A.Nazarov**, F.Brandstaetter*, T.Ntaflos*** and C.Koeberl****; (*) Naturhistorisches Muse

Add to Reading List

Source URL: www.lpi.usra.edu

Download Document from Source Website

File Size: 147,07 KB

Share Document on Facebook

Similar Documents

Geoengineering potential of artificially enhanced silicate weathering of olivine Peter Köhlera,1, Jens Hartmannb, and Dieter A. Wolf-Gladrowa a Alfred Wegener Institute for Polar and Marine Research (AWI), P.O. Box 12 0

Geoengineering potential of artificially enhanced silicate weathering of olivine Peter Köhlera,1, Jens Hartmannb, and Dieter A. Wolf-Gladrowa a Alfred Wegener Institute for Polar and Marine Research (AWI), P.O. Box 12 0

DocID: 1rOcv - View Document

46th Lunar and Planetary Science Conferencepdf SILICON CONDENSATION IN TYPE 1AB CHONDRULES AT NEAR EQUILIBRIUM CONDITIONS. E. R. Harju,1 I. E. Kohl1, A. E. Rubin1, and E. D. Young1, 1Department of Earth, Pl

46th Lunar and Planetary Science Conferencepdf SILICON CONDENSATION IN TYPE 1AB CHONDRULES AT NEAR EQUILIBRIUM CONDITIONS. E. R. Harju,1 I. E. Kohl1, A. E. Rubin1, and E. D. Young1, 1Department of Earth, Pl

DocID: 1rqW8 - 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

Project EARTH-16-LH3: Transient deformation of olivine: From seismic wave speeds to glacial isostacy Supervisor: Dr Lars Hansen The deformation behaviour of rocks is a strong function of timescale. On short timescales (s

Project EARTH-16-LH3: Transient deformation of olivine: From seismic wave speeds to glacial isostacy Supervisor: Dr Lars Hansen The deformation behaviour of rocks is a strong function of timescale. On short timescales (s

DocID: 1qXKd - View Document

44th Lunar and Planetary Science Conferencepdf RELATIVE SENSITIVITY FACTOR DEFINED FOR 53Mn-53Cr CHRONOMETRY OF SECONDARY FAYALITE. P. M. Doyle1,2*, K. Nagashima2, K. Jogo2, and A. N. Krot1,2. 1University o

44th Lunar and Planetary Science Conferencepdf RELATIVE SENSITIVITY FACTOR DEFINED FOR 53Mn-53Cr CHRONOMETRY OF SECONDARY FAYALITE. P. M. Doyle1,2*, K. Nagashima2, K. Jogo2, and A. N. Krot1,2. 1University o

DocID: 1qEws - View Document