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Mark A. Evans
Associate
Professor of Geology
Central Connecticut State University
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Research |
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Areas of Interest:
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Structural Geology |
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Rock strain and deformation
mechanisms |
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Paleofluid evolution and migration |
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Paleohydrostrtigraphy |
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Paleomagnetism and AMS |
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History of Geology |
My primary area of interest is establishing environmental
conditions (pressure, temperature, strain rate, and stress) of
deformation in orogenic belts. I am particularly interested in
applying deformation mechanism regimes, strain partitioning,
metamorphic petrology, and fluid inclusion analysis to determine these
conditions. More recently, my research has focused on paleofluid
evolution and migration, and the relationship of paleofluid flow to
paleo-remagnetization events.
Specific Areas:
- Fluid evolution and migration in a foreland
fold-and-thrust belt. Previous work has resulted in determining the
paleohydrologic structure of the central Appalachian Valley and
Ridge province during the Alleghanian orogeny. This was accomplished
by analyzing fluid inclusions, stable isotopes, and geochemistry of
fracture and vein mineral fillings in order to trace temporal and
areal variations in paleofluid chemistry. The Petroleum Research
Fund is currently supporting an extension of this study into the
surface and subsurface rocks of the Plateau province. Eventually, I
am planning to extend this study into the Blue Ridge and Piedmont in
order to ultimately gain a complete picture of fluid evolution in
the orogen.
- Investigation of the Late Paleozoic remagnetization
event in the central Appalachians. Related to the above project is a
current study in collaboration with Dr. Douglas Elmore (University
of Oklahoma) to investigate the relationship between paleofluid flow
and remagnetization. Many workers have related the remagnetization
event to the passage of ‘warm’ exotic fluids from the hinterland.
However our work to date indicates that this relationship may not
exist. Instead, the remagnetization may be related of hydrocarbon
generation, strain, or diagenetic rock alteration. Associated with
this project, we are examining the distribution of magnetic grains
in rock and how they are modified with rock strain. This work is
supported by the National Science Foundation.
- Determining the paleofluid evolution in the eastern
Piedmont (Savannah River site area) of South Carolina and Georgia.
This work involves establishing the age relationships of brittle
structures in the Piedmont rocks and the overlying Coastal Plain
sediments, and fluid inclusion studies of vein filling minerals.
This work is done in collaboration with Dr. Jerry Bartholomew
(University of Memphis). This work was supported by the U.S.
Department of Energy
- Examining paleo-fluids in the Sawtooth Range thrust
system in northwestern Montana. The goal is to understand fluid
evolution and migration during thrust faulting. In addition, I am
examining the relationship of fluids to rock remagnetization. This
work is in collaboration with Dr. Douglas Elmore (University of
Oklahoma).
- The relationship between fluids and deformation in the
Sierra Madre Oriental of Mexico. This project is in collaboration
with Mark Fisher (Northern Illinois). The goal is to examine the
deformation in the rocks, determine pressure-temperature conditions
from fluid inclusions in veins, and relate that information to
deformation mechanisms.
An overview of my Central Appalachian paleofluid
research An overview of my rock magnetism research
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