Bryn Mawr College
Department of Geology
Bryn Mawr, PA 19010
Office Location: 294 Park Science Building
Phone: (610)526-5111
Fax: (610)526-5086
email: mcrawfor(at)brynmawr.edu
WebPage: www.brynmawr.edu/geology/MLC/
Mineralogy, igneous and metamorphic petrology, and Tectonics
My research is solving the
history of mountain belts (such as the Coast Orogen of British Columbia and
southeastern Alaska or the older Appalachians in Pennsylvania) by looking at as
many different aspects as possible of the kinds of rocks, the time the rocks
formed, the location in which they formed, the way the earth moved. The total
time span for the mountain belt I study in British Columbia is from 110 million
years ago to the present.
A bimodal volcanic–plutonic
system: the Zarembo Island extrusive suite and the Burnett Inlet intrusive
complex. Lindline, Jennifer, Crawford, W.A. and Crawford,
M.L., Canadian Journal of Earth Sciences, v. 41, p. 355-375.
Using incongruent, equilibrium
hydration reactions to model latter-stage crystallization in plutons: examples
from the Bell Island tonalite, Alaska. Beard, J.S., Ragland, P.C., and
Crawford, M.L. Journal of Geology, v. 113, 589-599.
Reactive bulk assimilation: A model for
crust-mantle mixing in silicic magmas. Beard, J.S., Ragland, P.C., and
Crawford, M.L. Geology: v. 33, 681–684.
105 million years of igneous
activity, Wrangell, Alaska, to Prince Rupert, British Columbia. Crawford,
M.L., Crawford, W.A. and Lindline, J. Canadian Journal of Earth Sciences,
v. 42, p. 1097-1116.
Paleomagnetism of Late Jurassic
to mid-Cretaceous plutons near Prince Rupert, British Columbia. Butler, R.F.,
Gehrels, G.E., Hart, W., Davidson, C. and Crawford, M.L.
In: Haggart, J.W., Enkin, R.J., Monger, J.W.H., eds., Paleogeography
of the North American Cordillera; evidence for and against large-scale displacements.
Geological Association of Canada Special Paper, vol. 46, pp.171-200, 200