Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas

Abstract

Research Article| September 01, 1986 Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas H. Martin H. Martin 1Centre Armoricain d'Etude Structurale des Socles, Institut de Géologie, Université de Rennes, 35042 Rennes Cédex, France Search for other works by this author on: GSW Google Scholar Geology (1986) 14 (9): 753–756. https://doi.org/10.1130/0091-7613(1986)14<753:EOSAGG>2.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation H. Martin; Effect of steeper Archean geothermal gradient on geochemistry of subduction-zone magmas. Geology 1986;; 14 (9): 753–756. doi: https://doi.org/10.1130/0091-7613(1986)14<753:EOSAGG>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The comparative study of Archean and post-Archean granitic rocks shows significant changes with time. The high rare-earth element fractionation and the low Yb content of the Archean granitoids indicate the major role of garnet and hornblende, whereas these two minerals do not play a prominent part in the genesis of modern granitic rocks. This difference is a direct consequence of the cooling of Earth.In Archean time the subducted oceanic crust was young and warm, so it reached the conditions of melting before dehydration had occurred, leaving a garnet- and hornblende-bearing residue. In contrast, the modern subducted oceanic slab is generally old and cold, so it is dehydrated before it reaches the melting conditions of hydrous tholeiite; therefore, in the absence of a hydrous phase, it cannot melt at shallow depth. The fluids produced by dehydration reactions of modern crust rehydrate the overlying mantle wedge, which, in consequence, can undergo partial melting and give rise to calc-alkaline magmas; in this case, olivine and pyroxene are the most important residual phases. The location of calc-alkaline magma genesis in subduction-zone environments has migrated over time from the subducted Archean oceanic crust to the mantle wedge, a migration attributed to the progressive cooling of Earth. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.