A conspicuous clay ovoid in Nakhla: evidence for subsurface hydrothermal alteration on Mars with implications for astrobiology. (2014)

First Author: Chatzitheodoridis E
Attributed to:  Investigating the Solar System with Isotope Cosmochemistry funded by STFC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1089/ast.2013.1069

PubMed Identifier: 25046549

Publication URI: http://europepmc.org/abstract/MED/25046549

Type: Journal Article/Review

Volume: 14

Parent Publication: Astrobiology

Issue: 8

ISSN: 1557-8070