Mechanics and mechanisms of magmatic underplating: inferences from mafic veins in deep crustal mylonite
Dioritic to gabbro-dioritic veins with extreme length to width ratios (>1000:1) are localized along an amphibolite facies shear zone (the CMB Line) between exposed segments of originally middle and lower continental crust (Strona-Ceneri and Ivrea-Verbano
|Collections||ANU Research Publications|
|Source:||Earth and Planetary Science Letters|
|01_Handy_Mechanics_and_mechanisms_of_1999.pdf||1.67 MB||Adobe PDF||Request a copy|
Items in Open Research are protected by copyright, with all rights reserved, unless otherwise indicated.