Mount Luyendyk
In December, 1989, geologists of the UC Santa Barbara FORCE expedition traveled by snowmobile-sledge to Mt. Luyendyk, for the purpose of sampling for rock magnetism, petrology, and geochronology studies. Between 2005 and 2012, geologists from Colorado College, University of Maryland, and Curtin University (Perth) returned to Mt. Luyendyk for structural geology and petrology investigations.
Geology
Mt. Luyendyk consists of migmatite gneiss and plutonic rocks within the Fosdick Mountains gneiss dome/core complex. The rocks constitute an exposure of the middle crust that was exhumed approximately 100 million years ago, during the Cretaceous Period, by action on the Fosdick Mountains detachment fault.
References
- ^ Siddoway, Christine (2004). "Origin and emplacement mechanisms for a middle Cretaceous gneiss dome, Fosdick Mountains, West Antarctica". GSA Special Paper. 380: 267–294. doi:10.1130/0-8137-2380-9.267.
- ^ McFadden, Rory (2010). "Oblique dilation, melt transfer, and gneiss dome emplacement". Geology. 38 (4): 375–378. Bibcode:2010Geo....38..375M. doi:10.1130/G30493.1.
External links
Geographic Names: http://geonames.usgs.gov/apex/f?p=gnispq:5:::NO::P5_ANTAR_ID:19588