{"id":2515,"date":"2019-10-02T19:54:51","date_gmt":"2019-10-02T19:54:51","guid":{"rendered":"https:\/\/www.gsnv.org\/shop\/the-evolution-and-relationship-of-the-western-north-american-paleozoic-carbonate-platform-and-basin-depositional-environments-to-carlin-type-gold-deposits-in-the-context-of-carbonate-sequence-stratigr\/"},"modified":"2020-02-24T18:18:00","modified_gmt":"2020-02-24T18:18:00","slug":"the-evolution-and-relationship-of-the-western-north-american-paleozoic-carbonate-platform-and-basin-depositional-environments-to-carlin-type-gold-deposits-in-the-context-of-carbonate-sequence-stratigr","status":"publish","type":"product","link":"https:\/\/www.gsnv.org\/shop\/the-evolution-and-relationship-of-the-western-north-american-paleozoic-carbonate-platform-and-basin-depositional-environments-to-carlin-type-gold-deposits-in-the-context-of-carbonate-sequence-stratigr\/","title":{"rendered":"The Evolution and Relationship of the Western North American Paleozoic Carbonate Platform and Basin Depositional Environments to Carlin-Type Gold Deposits in the Context of Carbonate Sequence Stratigraphy"},"content":{"rendered":"","protected":false},"excerpt":{"rendered":"<p>The Western North American continent developed by passive-margin rifting<br \/>\nfrom a Late Proterozoic supercontinent. This breakup formed a ~5,000-km-long passive<br \/>\ncontinental margin from the Late Proterozoic (~600 Ma) through the Devonian<br \/>\n(~360 Ma), upon which a ~15,000\u201320,000 foot-thick (~4,500\u20136,000 m) carbonate platform<br \/>\nand basin formed. Carbonate sequence stratigraphy is a powerful tool to understand<br \/>\nhow this carbonate platform and basin evolved.<\/p>\n","protected":false},"featured_media":4325,"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\/2515"}],"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=2515"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media\/4325"}],"wp:attachment":[{"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/media?parent=2515"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_cat?post=2515"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/www.gsnv.org\/wp-json\/wp\/v2\/product_tag?post=2515"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}