Oceanic Crust When Earth Was Young
- 11 May 2001
- journal article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 292 (5519) , 1076-1079
Abstract
Oceanic crust covers two-thirds of Earth9s rigid outer layer, and this was probably already the case during the Archean (over 2500 million years ago), when heat flow from Earth9s interior was much higher than today. It is believed that oceanic crust generated in the Archean differed from that produced today, but evidence has been hard to come by. In his Perspective, Karson highlights a report by Kusky et al., who have found the best candidate for Archean oceanic crust to date. This ophiolite complex appears to include a complete section of ancient submarine lavas to upper mantle material. It may allow some of the ideas regarding Archean tectonics and the ancient mid-ocean ridge biosphere to be tested.Keywords
This publication has 9 references indexed in Scilit:
- The Archean Dongwanzi Ophiolite Complex, North China Craton: 2.505-Billion-Year-Old Oceanic Crust and MantleScience, 2001
- Archean Greenstone Belts Are Not Oceanic CrustThe Journal of Geology, 1994
- Variations in thickness of layer 3 dominate oceanic crustal structureEarth and Planetary Science Letters, 1993
- The Volume and Composition of Melt Generated by Extension of the LithosphereJournal of Petrology, 1988
- Implications of melting for stabilisation of the lithosphere and heat loss in the ArchaeanEarth and Planetary Science Letters, 1986
- Archaean plate tectonics revisited 1. Heat flow, spreading rate, and the age of subducting oceanic lithosphere and their effects on the origin and evolution of continentsTectonics, 1984
- origin and emplacement of ophiolitesReviews of Geophysics, 1982
- Archean Plate Tectonics: Constraints and InferencesThe Journal of Geology, 1982
- Were Archean continental geothermal gradients much steeper than those of today?Nature, 1978