Research work · 1994

Evolution of the Slave craton

Clark E. Isachsen, Samuel A. Bowring

Geology

Abstract

Research Article| October 01, 1994 Evolution of the Slave craton C. E. Isachsen; C. E. Isachsen 1Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139 Search for other works by this author on: GSW Google Scholar S. A. Bowring S. A. Bowring 1Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139 Search for other works by this author on: GSW Google Scholar Geology (1994) 22 (10): 917–920. https://doi.org/10.1130/0091-7613(1994)022<0917:EOTSC>2.3.CO;2 Article history first online: 02 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 C. E. Isachsen, S. A. Bowring; Evolution of the Slave craton. Geology 1994;; 22 (10): 917–920. doi: https://doi.org/10.1130/0091-7613(1994)022<0917:EOTSC>2.3.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 Greenstone belts in the Slave craton represent the episodic accumulation of volcanic and sedimentary rocks over as much as 200 m.y. In the western craton, volcanic and sedimentary rocks were deposited between 2.81 and 2.60 Ga on 2.9->3.1 Ga sialic basement, not tectonically juxtaposed with it. Deposition of 2.6 Ga turbidite and conglomerate sequences across the entire Slave craton was synchronous with, or followed by, the main phase of regional deformation and metamorphism at 2.6-2.58 Ga and final stabilization of the craton. 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.

DOI: 10.1130/0091-7613(1994)022<0917:eotsc>2.3.co;2