year 3, Issue 2 (Summer 2013 2013)                   E.E.R. 2013, 3(2): 27-37 | Back to browse issues page

XML Persian Abstract Print

Download citation:
BibTeX | RIS | EndNote | Medlars | ProCite | Reference Manager | RefWorks
Send citation to:

Development of Spheroidal Weathering and Exfoliation (Onion- Skin Erosion) In Dioritic-Quartz Dioritic Massifs of Ghaleh Ganj-Kerman. E.E.R. . 2013; 3 (2) :27-37
Abstract:   (4623 Views)

       The Ghaleh Ganj dioritic- quartz dioritic massifs, as a part of intrusive in the Makran zone show spheroidal weathering and exfoliation. This phenomenon is related to the development of micro-crack systems. Furthermore, various factors such as mechanical properties of rock-forming minerals, tectonic stresses, increasing volume during mineral weathering and earth surface temperature fluctuations may be important in the formation of these features. It seems that the presence of feldspar, biotite and secondary minerals (such as clay minerals, secondary biotite and Fe- oxides) in the study area, played an important role in the development of spheroidal weathering and exfoliation. However, the modal contents of biotite is the main controlling factor.

Full-Text [PDF 698 kb]   (1378 Downloads)    
Type of Study: Research |
Received: 2014/06/10 | Published: 2014/06/10

Add your comments about this article : Your username or Email:
Write the security code in the box

© 2018 All Rights Reserved | Environmental Erosion Research Journal

Designed & Developed by : Yektaweb