The Echo Cliff structure: identification and analysis of a possible Kansan impact structure

dc.contributor.authorLane, Adam Eldon
dc.date.accessioned2018-04-20T20:46:47Z
dc.date.available2018-04-20T20:46:47Z
dc.date.graduationmonthMayen_US
dc.date.issued2018-05-01en_US
dc.date.published2018en_US
dc.description.abstractThis study examines an ovoid drainage feature southwest of Topeka, Kansas, whose discovery sparked a flurry of activity. Geomicrobial and surface gamma ray surveys indicated possible vertical migration of hydrocarbons, and a ground magnetic survey produced anomalies that resemble the profile of a crater. The area was dubbed the Echo Cliff structure and considered analogous to the Ames structure in Oklahoma, an Ordovician impact structure remarkable for significant hydrocarbon recovery. However, four wells drilled in the area were dry and abandoned. The Echo Cliff structure did yield further indications of its origins by the discovery of possible shocked quartz in drill cuttings from the Ordovician Simpson Group. Our study integrated well log analysis, geophysical modeling, and petrographic analysis to verify or refute the proposed identity of the Echo Cliff structure. Well logs from the area were used to create a structural and stratigraphic cross-section in Petrel® 2016. A gravity survey was conducted in the study area and combined with an aeromagnetic survey, donated by Applied Geophyics, Inc., to use as the basis for geophysical modeling within GM-SYS®. Finally, drill cuttings from the Simpson Group of two wells in the study area were mounted for thin sectioning. These thin sections were examined for planar deformation features, which are indicative of an impact event. The structural and stratigraphic cross sections indicated minimal variation in the subsurface, which is uncharacteristic of an impact event. The GM-SYS® geophysical models seem to indicate that variations in the topography of the Precambrian basement and faulting from the Bolivar-Mansfield Tectonic Zone are responsible for the geophysical anomalies and possibly the current drainage pattern of the study area. Finally, no planar deformation features were observed in any of the examined thin sections. Therefore, there is currently no evidence in support of the claim that the Echo Cliff structure is an impact structure.en_US
dc.description.advisorAbdelmoneam Raefen_US
dc.description.advisorMatthew W. Tottenen_US
dc.description.degreeMaster of Scienceen_US
dc.description.departmentDepartment of Geologyen_US
dc.description.levelMastersen_US
dc.description.sponsorshipAAPG Foundationen_US
dc.identifier.urihttp://hdl.handle.net/2097/38882
dc.language.isoen_USen_US
dc.subjectImpact structureen_US
dc.subjectEcho Cliffen_US
dc.subjectGravity surveyen_US
dc.subjectShocked quartzen_US
dc.subjectGeophysical modelen_US
dc.subjectBolivar-Mansfield Tectonic Zoneen_US
dc.titleThe Echo Cliff structure: identification and analysis of a possible Kansan impact structureen_US
dc.typeThesisen_US

Files

Original bundle
Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
AdamLane2018.pdf
Size:
7.01 MB
Format:
Adobe Portable Document Format
Description:
License bundle
Now showing 1 - 1 of 1
No Thumbnail Available
Name:
license.txt
Size:
1.62 KB
Format:
Item-specific license agreed upon to submission
Description: