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University of Kentucky

Earth and Environmental Sciences Faculty Publications

2014

Articles 1 - 3 of 3

Full-Text Articles in Physical Sciences and Mathematics

Vegetation Controls On Weathering Intensity During The Last Deglacial Transition In Southeast Africa, Sarah J. Ivory, Michael M. Mcglue, Geoffrey S. Ellis, Anne-Marie Lézine, Andrew S. Cohen, Annie Vincens Nov 2014

Vegetation Controls On Weathering Intensity During The Last Deglacial Transition In Southeast Africa, Sarah J. Ivory, Michael M. Mcglue, Geoffrey S. Ellis, Anne-Marie Lézine, Andrew S. Cohen, Annie Vincens

Earth and Environmental Sciences Faculty Publications

Tropical climate is rapidly changing, but the effects of these changes on the geosphere are unknown, despite a likelihood of climatically-induced changes on weathering and erosion. The lack of long, continuous paleo-records prevents an examination of terrestrial responses to climate change with sufficient detail to answer questions about how systems behaved in the past and may alter in the future. We use high-resolution records of pollen, clay mineralogy, and particle size from a drill core from Lake Malawi, southeast Africa, to examine atmosphere-biosphere-geosphere interactions during the last deglaciation (~ 18-9 ka), a period of dramatic temperature and hydrologic changes. The …

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Northeast‐Oriented Transpression Structure In The Northern New Madrid Seismic Zone: Extension Of A Shear Zone Across The Reelfoot Fault Stepover Arm, Edward W. Woolery, Ali Almayahi Oct 2014

Northeast‐Oriented Transpression Structure In The Northern New Madrid Seismic Zone: Extension Of A Shear Zone Across The Reelfoot Fault Stepover Arm, Edward W. Woolery, Ali Almayahi

Earth and Environmental Sciences Faculty Publications

High‐resolution seismic‐reflection profiles recently acquired 12 km northeast of the New Madrid seismic zone’s Reelfoot thrust and along the central axis of the Reelfoot rift, imaged steeply dipping N30°E striking faults that have uplifted and arched post‐Paleozoic sediments in a manner consistent with a dextral strike‐slip component of displacement. The subparallel fault strands have been traced 1.4 km between reflection profiles. In order to evaluate the structure’s potential regional scale, the strike was projected northeast 22 km to its intersection with a nearby industry profile. At the intersection, this lower‐resolution profile exhibits a discrete 0.75 km wide structure with style …

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The MW 4.2 Perry County, Kentucky, Earthquake Of 10 November 2012: Evidence Of The Eastern Tennessee Seismic Zone In Southeastern Kentucky, N. Seth Carpenter, Edward W. Woolery, Zhenming Wang Jul 2014

The MW 4.2 Perry County, Kentucky, Earthquake Of 10 November 2012: Evidence Of The Eastern Tennessee Seismic Zone In Southeastern Kentucky, N. Seth Carpenter, Edward W. Woolery, Zhenming Wang

Earth and Environmental Sciences Faculty Publications

The 10 November 2012 Mw 4.2 Perry County earthquake may represent a continuation of the seismically active Eastern Tennessee seismic zone (ETSZ) farther north than previously recognized into southeastern Kentucky. The mainshock and aftershock data from regional seismic networks and EarthScope’s Transportable Array stations allowed high‐quality determinations of the source parameters. The focal mechanism, depth, and proximity of the mainshock to the New York–Alabama magnetic lineament, a subsurface, crustal‐scale structure that spatially correlates with central ETSZ seismicity, suggest that this earthquake may share the same type of causal geologic structures as the more‐active ETSZ region to the south.

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