|2006 Philadelphia Annual Meeting (22–25 October 2006)|
|Paper No. 21-4|
|Presentation Time: 9:00 AM-9:15 AM|
FORMATION AND EMPLACEMENT OF IMPACT BRECCIAS IN CARBONATE TARGET ROCKS: EXAMPLES FROM SOUTHERN MISSOURI
EVANS, Kevin R., Geography, Geology, & Planning, Missouri State University, 901 S. National Ave, Springfield, MO 65897, email@example.com, MILLER, James F., Geography, Geology, & Planning, Missouri State University, Springfield, MO 65897, MULVANY, Patrick S., Missouri Department of Natural Resources, Division of Geology and Land Survey, 111 Fairgrounds Rd, Rolla, MO 65401, and DAVIS, George H., Missouri Department of Transportation, 1617 Missouri Blvd, Jefferson City, MO 65102|
Two widely accepted impact structures are located in southern Missouri: Decaturville (7 km dia.) and Crooked Creek (6 km dia.). The Weaubleau structure (8 km dia.) is another area of locally anomalous intense structural deformation. Planar lamellae in quartz grains from the “Weaubleau Breccia” are consistent with an impact origin and further analyses are underway. Collectively, these structures contain a variety of breccias that differ in the timing of their formation during the cratering process and in their modes of deposition or emplacement.
Principal breccia types include (1) fracture breccia, (2) megabreccia, (3) injection breccia, (4) dilation breccia, (5) crystalline basement breccia, and (6) ejecta/resurge breccia. The distinction between fracture breccia and megabreccia is arbitrarily placed at 1.0 m clast size, but the mode of formation and emplacement is essentially the same. Both are found in central uplift areas and in material-flow debris blankets in crater moat regions. Fracture breccia and megabreccia clasts rest in a comminution matrix or are surrounded by injection breccia. Injection breccia appears to have a fluid matrix that formed and was emplaced at depth during the excavation and modification stages. Dilation breccia, known only from the Weaubleau structure, essentially formed in situ during the excavation stage but may have been transported en mass during the modification stage. Granitic and pegmatitic clasts in the Decaturville and Weaubleau structures indicate deep penetration and uplift associated with formation of crystalline basement breccia. The uppermost part of the “Weaubleau Breccia” is a carbonate-matrix-supported breccia that exhibits coarse grading associated with deposition in a marine setting.
The primary factor in the preservation of different breccia types at each of Missouri structure is related to the depth of post-impact erosion. The ejecta/resurge facies of the Weaubleau Breccia was buried below limestones of the Meramecian Warsaw and Salem formations prior to subaerial exposure, karstification, dissolution of overlying limestones, and subsequent re-burial by Pennsylvanian strata. Most of the middle and late Paleozoic strata have been eroded from the Decaturville and Crooked Creek structures.
2006 Philadelphia Annual Meeting (22–25 October 2006)
General Information for this Meeting
|Session No. 21|
Terrestrial Impact Breccias
Pennsylvania Convention Center: 112 A
8:00 AM-12:00 PM, Sunday, 22 October 2006
Geological Society of America Abstracts with Programs, Vol. 38, No. 7, p. 58
© Copyright 2006 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.