Anomalous Thermal Indicators from
Authigenic Minerals in Upper
Paleozoic Strata of the Michigan Basin
Kyle J. Cox
Western Michigan University
Authigenic mineralization and thermally mature organic material requiring
anomalously high paleo-temperatures have been found throughout the Michigan
basin. Numerous explanations have been proposed to explain these diagenetic
features: an elevated paleo-geothermal gradient, 2 km of post-Pennsylvanian
overburden, and hydrothermal fluids from
the Mid-Continent Rift found under the
basin travelling up through faults and fractures. None has been proven
conclusively. Additional investigation into the distribution of these anomalies, the
temperature at which they formed, and when they formed is required to
determine the mechanism of their creation. Information
from
the Mississippian
and Pennsylvania strata of the basin is especially deficient, but previous
investigations have identified abnormal diagenetic features within these shallow
formations. This project proposes to test the hypothesis that these diagenetic
features are related to the Mid-Continent Rift while providing additional data
from
an under investigated section of the basin. This will be accomplished through:
identification of samples
from
Upper Paleozoic formations with diagenetic
indications of elevated paleo-temperatures through X-ray
diffraction
and
petrographic observation, determination of the temperature of formation for these
features through fluid inclusion and isotopic analysis, dating the time of formation
through K-Ar age dating, and mapping the results for comparison with the
location of the Mid-Continent Rift and associated structures to determine a
correlation.
AAPG Search and Discovery Article #90182©2013 AAPG/SEG Student Expo, Houston, Texas, September 16-17, 2013