METEORITE
Abstract: Small circular hollows are very common in the glacial topography of NW Poland. Among them there are also some of meteorite origin. An important example of impact craters exists in the Morasko Meteorite Natural Reserve. The 14C and Luminescence datings are very helpful in establishing their...
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.8093 http://www.geochronometria.pl/pdf/geo_20/geo_20_17.pdf |
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.549.8093 2023-05-15T16:37:36+02:00 METEORITE Wojciech Stankowski The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.8093 http://www.geochronometria.pl/pdf/geo_20/geo_20_17.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.8093 http://www.geochronometria.pl/pdf/geo_20/geo_20_17.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.geochronometria.pl/pdf/geo_20/geo_20_17.pdf text ftciteseerx 2016-01-08T11:27:37Z Abstract: Small circular hollows are very common in the glacial topography of NW Poland. Among them there are also some of meteorite origin. An important example of impact craters exists in the Morasko Meteorite Natural Reserve. The 14C and Luminescence datings are very helpful in establishing their origin. The last ice sheet retreat and permafrost degradation cre-ated kettle-like hollows around the Morasko Hill. Organic infilling started in them between 14,000 10,000 BP. The Morasko meteorite shower fell between 5000 3500 BP. The craters origins and young hollow bottom organic infillings then started. On the Great Poland Lowland there are other potential areas with forms connected to mete-orite falls, the such as Oborniki- Obrzycko area and probably in the so called KKR object fron the south-east part of Great Poland Lowland. Key words: Text Ice Ice Sheet permafrost Unknown Fron ENVELOPE(-21.900,-21.900,64.142,64.142) |
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Open Polar |
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Unknown |
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ftciteseerx |
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English |
| description |
Abstract: Small circular hollows are very common in the glacial topography of NW Poland. Among them there are also some of meteorite origin. An important example of impact craters exists in the Morasko Meteorite Natural Reserve. The 14C and Luminescence datings are very helpful in establishing their origin. The last ice sheet retreat and permafrost degradation cre-ated kettle-like hollows around the Morasko Hill. Organic infilling started in them between 14,000 10,000 BP. The Morasko meteorite shower fell between 5000 3500 BP. The craters origins and young hollow bottom organic infillings then started. On the Great Poland Lowland there are other potential areas with forms connected to mete-orite falls, the such as Oborniki- Obrzycko area and probably in the so called KKR object fron the south-east part of Great Poland Lowland. Key words: |
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The Pennsylvania State University CiteSeerX Archives |
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Text |
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Wojciech Stankowski |
| spellingShingle |
Wojciech Stankowski METEORITE |
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Wojciech Stankowski |
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Wojciech Stankowski |
| title |
METEORITE |
| title_short |
METEORITE |
| title_full |
METEORITE |
| title_fullStr |
METEORITE |
| title_full_unstemmed |
METEORITE |
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meteorite |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.8093 http://www.geochronometria.pl/pdf/geo_20/geo_20_17.pdf |
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ENVELOPE(-21.900,-21.900,64.142,64.142) |
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Fron |
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Fron |
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Ice Ice Sheet permafrost |
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Ice Ice Sheet permafrost |
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http://www.geochronometria.pl/pdf/geo_20/geo_20_17.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.549.8093 http://www.geochronometria.pl/pdf/geo_20/geo_20_17.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766027893216903168 |