Use of Tmax as a thermal maturity indicator in orogenic successions and comparison with clay mineral evolution

Author: Dellisanti F.   Pini G. A.   Baudin F.  

Publisher: Mineralogical Society

ISSN: 1471-8030

Source: Clay Minerals, Vol.45, Iss.1, 2010-03, pp. : 115-130

Disclaimer: Any content in publications that violate the sovereignty, the constitution or regulations of the PRC is not accepted or approved by CNPIEC.

Previous Menu Next

Abstract