An alkaline spring system within the Del Puerto Ophiolite (California, USA): A Mars analog site

Planetary and Space Science

Volumn 57, Issue 5-6, 2009, Pages 533-540

  Blank, J G ^a,b   Green, S J ^b   Blake, D ^b   Valley, J W ^c   Kita, N T ^c   Treiman, A ^d   Dobson, P F ^e  

^a SETI INSTITUTE   (United States)

^b NASA AMES RESEARCH CENTER   (United States)

^c UNIVERSITY OF WISCONSIN MADISON   (United States)

^d LUNAR AND PLANETARY INSTITUTE   (United States)

^e LAWRENCE BERKELEY NATIONAL LABORATORY   (United States)

Author keywords

Alkaline springs; Biosignature; Dolomite; Mars analog

Indexed keywords

ABIOGENIC; ALKALINE SPRINGS; AQUEOUS GEOCHEMISTRIES; BEARING SYSTEMS; BIOSIGNATURE; CALIFORNIA; CALIFORNIA , USA; CANYON WALLS; CARBONATE CEMENTS; DOLOMITE; HYDROGEN GAS; LIFE ON MARS; MARS ANALOG; MARTIAN ATMOSPHERES; MICROBIAL COMMUNITIES; NEAR-SURFACE REGIONS; OCEANIC CRUSTS; PH VALUES; SERPENTINIZATION; SPRING SYSTEMS; SURFACE OF MARS; ULTRAMAFIC ROCKS; UPPER MANTLES;

ANALYTICAL GEOCHEMISTRY; CALCIUM; CRYSTALLOGRAPHY; HYDROGEN; LITHOLOGY; METHANE; MINERALOGY; MINERALS; OLIVINE; SILICATE MINERALS;

ROCKS;

EID: 67349201745     PISSN: 00320633     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pss.2008.11.018     Document Type: Article

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