WebGeology. Geologically the Great Dyke is not a dyke, but is lopolithic and Y-shaped in cross-section. It is a group of layered ultramafic intrusions that extend across Zimbabwe with a strike of about N10°E. The width of the intrusions vary from 3 to 12 km (7.5 mi). The Great Dyke is unusual in that most ultramafic layered intrusions display ... WebPREFACE. Welcome to the Pre-Symposium Excursion to the Great Dyke of Zimbabwe .sponsored and org.ani?.ed hy the Geolog.Ical Society of Zimbabwe as part, and on lx·hal!'. uf the 8th lntemational Platinum SvmposiUilL Rustenbnrg, South Africa 28th June to 3rd July, 1998.. The Great Dvke Is one ol several major maCic layered intrusions wurlcl …
Dike igneous rock Britannica
WebThe Great Dyke of Zimbabwe is a layered intrusion of igneous, metal-bearing rock that has been dated to approximately 2.5 billion years in age. ... This geological feature extends more than 550 kilometers (342 miles) … WebSep 1, 2003 · Re-Os data for chromite separates from 10 massive chromitite seams sampled along the 550-km length of the 2.58-Ga Great Dyke layered igneous complex, Zimbabwe, record initial 187Os/188Os ratios in ... its technical recruitment
Great Dyke, Zimbabwe - NASA
WebJan 1, 2011 · The Great Dyke of Zimbabwe hosts the world's second largest reserve of platinum-group elements (PGE). Economic PGE mineralization is restricted to sulfide … WebMay 1, 1982 · A. H. WILSON, The Geology of the Great ‘Dyke’, Zimbabwe: The Ultramafic Rocks, Journal of Petrology, Volume 23, Issue 2, May 1982, Pages 240–292, ... none of … WebMar 1, 2000 · The Great Dyke and its two main satellites, the Umvimeela and East Dykes, trend in a north—northeast direction across Archaean basement rocks of the Zimbabwe Craton. SHRIMP analysis of baddeleyite from all three intrusions yields statistically identical results and confirms their essentially synchronous emplacement at 2574 ±2 Ma. its technologies and logistics locations