- Amelia Creek crater
Amelia Creek crater is an
impact structure (orastrobleme ), the eroded remnant of a formerimpact crater , located in the Davenport Range,Northern Territory ,Australia . It lies within a low range ofPaleoproterozoic sedimentary and volcanic rocks, which are extensively folded and faulted, thus making an eroded impact crater difficult to recognize. It was only discovered by the identification of shatter cones near its centrecite journal | author=Macdonald FA, Mitchell K | title=Amelia Creek, Northern Territory, Australia: a 20 x 12 km oblique impact structure with no central uplift | journal=Impact Cratering: Bridging the Gap Between Modeling and Observations, February 2003, Houston, Texas, Lunar and Planetary Institute Contribution 1155 | volume= | issue= | year=2003 | pages=47 | id= [http://www.lpi.usra.edu/meetings/impact2003/pdf/8006.pdf Conference abstract] ] . The central shatter cone locality is surrounded by a 20 x 12 km area of anomalous deformation, the asymmetry being possibly related to very oblique impact, but may be at least partly due to the pre-existing structural complexity of the rockscite journal | author=Macdonald FA, Mitchell K, Stewart AJ | title=Amelia Creek: a Proterozoic impact structure in the Davenport Ranges, Northern Territory | journal=Australian Journal of Earth Sciences | volume=52 | issue= | year=2005 | pages=631–640 | id= | doi=10.1080/08120090500170401 [http://journalsonline.tandf.co.uk/link.asp?id=p4mt8066058648u8 Abstract] ] . This deformed zone gives the best estimate for the original size of the crater. Impact took place after folding of the Paleoproterozoic rocks but before deposition ofNeoproterozoic andCambrian rocks which overlie them, thus constraining the impact event to the interval between about 1660 and 600 Ma ] .References
External links
* [http://www.unb.ca/passc/ImpactDatabase/images/AmeliaCreek.html Amelia Creek at Earth Impact Database]
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