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	Por Dr. Wolfgang Griem ; Universidad de Atacama /Chile

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Metamorphism of mafic dikes from the central White-Inyo Range,
eastern California
W. G. Ernst
Department of Geological and Environmental Sciences, Stanford University, Stanford, CA 94305-2115, USA
Received: 13 March 1996 / Accepted: 24 December 1996
http://link.springer.de/link/service/journals/00410/bibs/7128001/71280030.htm

Paleomagnetic and 40Ar/39Ar
Geochronologic Data from
Late Proterozoic Mafic Dikes and Sills,
Montana and Wyoming
U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1580
By Stephen S. Harlan, John Wm. Geissman, and Lawrence W. Snee
http://greenwood.cr.usgs.gov/pub/ppapers/p1580/

Dike emplacement:
Experimental model showing growth of faults above dike
Photographs of cracking and faulting that occurred below the surface during a series of experiments
designed to simulate the intusion of magma along a dike. The dark area at the bottom of image is the
dike. The dark layers are corn meal and light layers consist of a 3:1 mixutre by volume of granualted
sugar and white flour. Obvious cracks (solid black lines) and less obvious cracks (dashed lines)
were mapped during the experiment. Note scale in lower right of photographs (2 cm scale). The
solid black line at the top of each photograph represents the original location of the
surface before the experiment began.
http://quake.wr.usgs.gov/VOLCANOES/LongValley/InyoEruption/fault_caption.html