subject predicate object context
24303 Creator bd12e480200a0e58504d6106bfed3c8a
24303 Creator ext-a48afdcafb09d9f0fa4a6b114a08ca4d
24303 Creator ext-c1f5811d4ff6811650e25768ec0d8e54
24303 Creator ext-c3bf42cf0a5ae6f17e4360a520443143
24303 Creator ext-eaafbb2a71b337bdb66d3665fc3fb3e7
24303 Date 2008
24303 Is Part Of repository
24303 abstract Ferropicrite basalts – basalts with relatively high-Fe and low-Al contents compared to ‘normal' basalts – are a minor but widespread component of magmatism on Earth. We have investigated how widespread high-Fe, low-Al compositions (similar to ferropicrites) are on other terrestrial planetary bodies and suggest that these basalts formed through similar processes.
24303 authorList authors
24303 presentedAt ext-0c8139f3f07e568ed598f64ad63634d8
24303 status nonPeerReviewed
24303 type AcademicArticle
24303 type Article
24303 label Filiberto, Justin; Kirchoff, Michelle R.; Schwenzer, Susanne P. ; Kieffer, Walter S. and Treiman, Allan H. (2008). High-Fe, low-Al basalts: evidence of extensive mantle processing on Earth, Moon, Mars, Vesta, Venus, and Io. In: Geological Society of America Annual Meeting, 5-9 Oct 2008, Houston TX.
24303 label Filiberto, Justin; Kirchoff, Michelle R.; Schwenzer, Susanne P. ; Kieffer, Walter S. and Treiman, Allan H. (2008). High-Fe, low-Al basalts: evidence of extensive mantle processing on Earth, Moon, Mars, Vesta, Venus, and Io. In: Geological Society of America Annual Meeting, 5-9 Oct 2008, Houston TX.
24303 Title High-Fe, low-Al basalts: evidence of extensive mantle processing on Earth, Moon, Mars, Vesta, Venus, and Io
24303 in dataset oro