Discriminating between impact or nonimpact origin of small meteorite crater candidates : No evidence for an impact origin for the Tor crater, Sweden
(2022) In Meteoritics and Planetary Science 57(11). p.1987-2002- Abstract
Compared to intensive research on km-sized meteorite impact craters, fewer studies focus on smaller craters. The small craters are often hard or impossible to recognize using “classical” criteria like the presence of shatter cones, shocked quartz, and geochemical indicators. Therefore, a long list of candidate structures awaiting approval/disapproval of their origin has been formed over the last decades. One of them is the Tor structure in central Sweden. To test a hypothesis of an impact origin of this structure, we have performed topographical analysis, geophysical studies, 10Be exposure dating of boulders, and 14C dating of Tor-associated charcoal. None of the methods gave us a reason to claim the Tor structure... (More)
Compared to intensive research on km-sized meteorite impact craters, fewer studies focus on smaller craters. The small craters are often hard or impossible to recognize using “classical” criteria like the presence of shatter cones, shocked quartz, and geochemical indicators. Therefore, a long list of candidate structures awaiting approval/disapproval of their origin has been formed over the last decades. One of them is the Tor structure in central Sweden. To test a hypothesis of an impact origin of this structure, we have performed topographical analysis, geophysical studies, 10Be exposure dating of boulders, and 14C dating of Tor-associated charcoal. None of the methods gave us a reason to claim the Tor structure is of impact origin. Thus, we support a recently suggested idea of Tor being formed by a grounded iceberg within a glacial lake.
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- author
- Plado, Jüri ; Losiak, Ania ; Jõeleht, Argo ; Ormö, Jens ; Alexanderson, Helena LU ; Alwmark, Carl LU ; Wild, Eva Maria ; Steier, Peter ; Awdankiewicz, Marek and Belcher, Claire
- organization
- publishing date
- 2022-11
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Meteoritics and Planetary Science
- volume
- 57
- issue
- 11
- pages
- 16 pages
- publisher
- Wiley-Blackwell
- external identifiers
-
- scopus:85139847311
- ISSN
- 1086-9379
- DOI
- 10.1111/maps.13914
- language
- English
- LU publication?
- yes
- id
- ddbb3ebc-d9db-4f4a-adc9-b92092efd19a
- date added to LUP
- 2023-01-23 08:57:31
- date last changed
- 2023-01-23 08:59:24
@article{ddbb3ebc-d9db-4f4a-adc9-b92092efd19a,
abstract = {{<p>Compared to intensive research on km-sized meteorite impact craters, fewer studies focus on smaller craters. The small craters are often hard or impossible to recognize using “classical” criteria like the presence of shatter cones, shocked quartz, and geochemical indicators. Therefore, a long list of candidate structures awaiting approval/disapproval of their origin has been formed over the last decades. One of them is the Tor structure in central Sweden. To test a hypothesis of an impact origin of this structure, we have performed topographical analysis, geophysical studies, <sup>10</sup>Be exposure dating of boulders, and <sup>14</sup>C dating of Tor-associated charcoal. None of the methods gave us a reason to claim the Tor structure is of impact origin. Thus, we support a recently suggested idea of Tor being formed by a grounded iceberg within a glacial lake.</p>}},
author = {{Plado, Jüri and Losiak, Ania and Jõeleht, Argo and Ormö, Jens and Alexanderson, Helena and Alwmark, Carl and Wild, Eva Maria and Steier, Peter and Awdankiewicz, Marek and Belcher, Claire}},
issn = {{1086-9379}},
language = {{eng}},
number = {{11}},
pages = {{1987--2002}},
publisher = {{Wiley-Blackwell}},
series = {{Meteoritics and Planetary Science}},
title = {{Discriminating between impact or nonimpact origin of small meteorite crater candidates : No evidence for an impact origin for the Tor crater, Sweden}},
url = {{http://dx.doi.org/10.1111/maps.13914}},
doi = {{10.1111/maps.13914}},
volume = {{57}},
year = {{2022}},
}