{"id":2466,"date":"2019-10-02T19:53:42","date_gmt":"2019-10-02T19:53:42","guid":{"rendered":"https:\/\/www.gsnv.org\/shop\/tectonostratigraphy-of-the-great-basin-from-the-antler-orogeny-through-pennsylvanian-time\/"},"modified":"2020-02-24T18:17:44","modified_gmt":"2020-02-24T18:17:44","slug":"tectonostratigraphy-of-the-great-basin-from-the-antler-orogeny-through-pennsylvanian-time","status":"publish","type":"product","link":"https:\/\/www.gsnv.org\/shop\/tectonostratigraphy-of-the-great-basin-from-the-antler-orogeny-through-pennsylvanian-time\/","title":{"rendered":"Tectonostratigraphy of the Great Basin from the Antler orogeny through Pennsylvanian time"},"content":{"rendered":"","protected":false},"excerpt":{"rendered":"

The Antler orogeny, recorded by the formation of a foreland basin in latest Devonian
\ntime, was followed by a series of distinct late Paleozoic orogenic events that affected
\nthe western margin of North America. These events can be recognized by angular
\nunconformities which locally trim folds or thrust faults, and which are commonly
\noverlain by orogenic conglomerates. The timing of the deformation can be precisely
\ndetermined biostratigraphically, by dating rocks above and belowthe unconformities.
\nThe late Paleozoic unconformities (and tectonic events they record) have been little
\nrecognized, in part due to broad application of stratigraphic terminology throughout
\nNevada. For example, in some cases a single formation name has been applied to rocks
\nboth above and belowan unconformity.Revision of late Paleozoic stratigraphic terminology
\nis therefore in order.<\/p>\n","protected":false},"featured_media":4505,"comment_status":"closed","ping_status":"closed","template":"","meta":{"pmpro_default_level":""},"product_cat":[154],"product_tag":[],"_links":{"self":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product\/2466"}],"collection":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/types\/product"}],"replies":[{"embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/comments?post=2466"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media\/4505"}],"wp:attachment":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media?parent=2466"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_cat?post=2466"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_tag?post=2466"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}