Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Burkhard O. Dressler"'
Publikováno v:
Meteoritics & Planetary Science. 39:857-878
The impact breccias encountered in drill hole Yaxcopoil-1 (Yax-1) in the Chicxulub impact structure have been subdivided into six units. The two uppermost units are redeposited suevite and suevite, and together are only 28 m thick. The two units belo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78c6a120d3e197a2a78b30eeafa4459d
https://doi.org/10.1111/j.1945-5100.2004.tb00935.x
https://doi.org/10.1111/j.1945-5100.2004.tb00935.x
Publikováno v:
Earth-Science Reviews. 60:147-174
The Sudbury Structure, formed by meteorite impact at 1850 Ma, consists of three major components: (1) the Sudbury Basin; (2) the Sudbury Igneous Complex, which surrounds the basin as an elliptical collar; and (3) breccia bodies in the footwall known
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4d85f56ee5776247ae40ffbe38faf0fd
https://doi.org/10.1016/s0012-8252(02)00091-0
https://doi.org/10.1016/s0012-8252(02)00091-0
Publikováno v:
Contributions to Mineralogy and Petrology. 130:275-287
The Slate Islands archipelago is believed to represent the central uplifted portion of a complex impact structure. Planar microstructures in quartz and feldspars and shock vitrification of rocks are the most common shock metamorphic features encounte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::726baa1f318018ca012b9293e4d8e185
https://doi.org/10.1007/s004100050365
https://doi.org/10.1007/s004100050365
Publikováno v:
Meteoritics & Planetary Science. 32:249-258
The Wanapitei impact structure is approximately 8 km in diameter and lies within Wanapitei Lake, approximately 34 km northeast of the city of Sudbury. Rocks related to the 37 Ma impact event are found only in Pleistocene glacial deposits south of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5fdc9efe97149d067712829361e81b8c
https://doi.org/10.1111/j.1945-5100.1997.tb01263.x
https://doi.org/10.1111/j.1945-5100.1997.tb01263.x
Publikováno v:
Impact Studies ISBN: 3540241817
Many large meteorite impact structures throughout the world host mineral resources that are either currently mined or have the potential to become important economic resources in the future. The giant Vredefort-Witwatersrand and Sudbury impact struct
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ef695f4581646c350140e43f8ccb6b1
https://doi.org/10.1007/3-540-27548-7_20
https://doi.org/10.1007/3-540-27548-7_20
The target rocks of the 30-32-km diameter Slate Islands impact structure in northern Lake Superior, Canada, are Archean supracrustal and igneous rocks and supracrustal Proterozoic rocks. Shatter cones, pseudotachylites, impact glasses, and microscopi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d58dfe3626775d88ee62ed803bb04acb
https://doi.org/10.1130/0-8137-2339-6.109
https://doi.org/10.1130/0-8137-2339-6.109
Publikováno v:
Geology. 25:666
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41f91361d672b0722b818c8354463910
https://doi.org/10.1130/0091-7613(1997)025<0666:ncotsi>2.3.co
https://doi.org/10.1130/0091-7613(1997)025<0666:ncotsi>2.3.co
Publikováno v:
Geology. 24:851
The Slate Islands in northern Lake Superior represent the eroded remains of a complex impact crater, originally approximately 32 km in diameter. New field studies there reveal allogenic crater fill deposits along the eastern and northern portions of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ad1eda77d9ac7668805cfc51f2938cd
https://doi.org/10.1130/0091-7613(1996)024<0851:ncotsi>2.3.co
https://doi.org/10.1130/0091-7613(1996)024<0851:ncotsi>2.3.co