{"id":11324,"date":"2017-01-26T14:55:52","date_gmt":"2017-01-26T13:55:52","guid":{"rendered":"http:\/\/karmaka.de\/?p=11324"},"modified":"2017-01-26T14:55:52","modified_gmt":"2017-01-26T13:55:52","slug":"a-previously-unrecognized-high-temperature-impactite-from-the-steen-river-impact-structure-alberta-canada","status":"publish","type":"post","link":"https:\/\/karmaka.de\/?p=11324","title":{"rendered":"A previously unrecognized high-temperature impactite from the Steen River impact structure, Alberta, Canada"},"content":{"rendered":"<p>E.Walton, A.Hughes, E.MacLagan, C.D.K.Herd, M.Dence<\/p>\n<p>Geology<br \/>\nDOI: 10.1130\/G38556.1<br \/>\nFirst Published on January 23, 2017 <\/p>\n<p><a href=\"http:\/\/geology.geoscienceworld.org\/content\/early\/2017\/01\/23\/G38556.1\" target=\"_blank\"><strong>LINK<\/strong><\/a><\/p>\n<p>&#8220;Here, we report a previously unrecognized impactite from the Steen River impact structure in Alberta, Canada, which was intersected by continuous diamond drill core into the allochthonous proximal deposits of this buried 25-km-diameter complex crater. A suite of high-temperature minerals defines the matrix, formed by grain growth in a solid state by static recrystallization of an originally clastic matrix, deposited at temperatures \u2265800 \u00b0C. This rock type is predominantly a result of the recrystallization of target material driven by the acceleration of hot gasses from volatilized sedimentary cover mixed with variably shocked crystalline basement. Approximately one-third of terrestrial impact structures occur in mixed target rocks; therefore, this type of impactite may be more common than previously realized. Contact metamorphism between entrained sedimentary target rocks and the juxtaposed hot matrix resulted in carbonate decomposition to form a rare spinel-group mineral, magnesioferrite. In crater environments, magnesioferrite has been found in the distal Chicxulub (Mexico) ejecta and may prove a novel indicator mineral for impact into carbonate-bearing target rocks.&#8221;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>E.Walton, A.Hughes, E.MacLagan, C.D.K.Herd, M.Dence Geology DOI: 10.1130\/G38556.1 First Published on January 23, 2017 LINK &#8220;Here, we report a previously unrecognized impactite from the Steen River impact structure in Alberta, Canada, which was intersected by&#8230;<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[90],"tags":[95,1447,3558,3557],"_links":{"self":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/11324"}],"collection":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=11324"}],"version-history":[{"count":1,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/11324\/revisions"}],"predecessor-version":[{"id":11325,"href":"https:\/\/karmaka.de\/index.php?rest_route=\/wp\/v2\/posts\/11324\/revisions\/11325"}],"wp:attachment":[{"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=11324"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=11324"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/karmaka.de\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=11324"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}