{"id":1605,"date":"2019-12-04T15:31:49","date_gmt":"2019-12-04T15:31:49","guid":{"rendered":"http:\/\/www.icterra.pt\/?p=1605"},"modified":"2019-12-04T15:32:26","modified_gmt":"2019-12-04T15:32:26","slug":"emplacement-mechanism-of-caria-vila-da-ponte-pluton-northern-portugal-building-and-internal-magmatic-record","status":"publish","type":"post","link":"https:\/\/www.icterra.pt\/legacy\/index.php\/2019\/12\/04\/emplacement-mechanism-of-caria-vila-da-ponte-pluton-northern-portugal-building-and-internal-magmatic-record\/","title":{"rendered":"Emplacement mechanism of Caria-Vila da Ponte Pluton (Northern Portugal): Building and internal magmatic record"},"content":{"rendered":"<div id=\"abssec0010\">\n<p>Gon\u00e7alves, A., Sant\u2019Ovaia, H., Noronha, F., 2019.\u00a0<span lang=\"EN-US\">Emplacement mechanism of Caria-Vila da Ponte Pluton (Northern Portugal): Building and internal magmatic record. J Struc Geol 124, 91-111<\/span>.<\/p>\n<p id=\"abspara0010\" style=\"text-align: justify;\">The late to post-tectonic <a title=\"Learn more about Peridotite from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/peridotite\">biotite<\/a> <a title=\"Learn more about Granite from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/granite\">granites<\/a> from Caria\u2013Vila da Ponte area were studied for their mineralogical, microstructural and petrophysical standpoint using <a title=\"Learn more about Magnetic Anisotropy from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/magnetic-anisotropy\">anisotropy of magnetic susceptibility<\/a> coupled to <a title=\"Learn more about Petrography from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/petrography\">petrography<\/a> and <a title=\"Learn more about Scanning Electron Microscopy from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/scanning-electron-microscopy\">scanning electron microscopy<\/a>. One main direction, N339\u00b0-345\u00b0E, of stretching magnetic <a title=\"Learn more about Lineation from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/lineation\">lineations<\/a>, was found indicating that the <a title=\"Learn more about Emplacement from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/emplacement\">emplacement<\/a> of these granites was tectonically controlled. Although, the Caria \u2013 CA (on the W) and Vila da Ponte -VP (on the E) granites outcrops in distinct bodies, the results pointed out similar petrographic and petrophysical characteristics for both. Thus, it is suggested that both granites belong to only one asymmetric <a title=\"Learn more about Laccolith from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/laccolith\">laccolith<\/a> with a deep root <a title=\"Learn more about Feeder from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/feeder\">feeder<\/a> zone located in VP <a title=\"Learn more about Massif from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/massif\">massif<\/a>. A five-stage model is proposed: (I) passive <a title=\"Learn more about Magma from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/magma\">magma<\/a> <a title=\"Learn more about Ascent from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/ascent\">ascent<\/a> along NNW-SSE deep faults and <em>in situ<\/em> doming emplacement recorded in the magnetic\/magmatic fabric; (II) after total <a title=\"Learn more about Crystallization from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/crystallization\">crystallization<\/a> of the <a title=\"Learn more about Pluton from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/pluton\">pluton<\/a>, a late alteration most evident in the VP granite, promoted a normal zoning of the <a title=\"Learn more about Magnetic Permeability from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/magnetic-permeability\">magnetic susceptibility<\/a>; (III) NNW-SSE to NNE-SSW regional faults promoted the uplift of the CA relatively to VP; (IV) laying of <a title=\"Learn more about Quartz Vein from ScienceDirect's AI-generated Topic Pages\" href=\"https:\/\/www.sciencedirect.com\/topics\/earth-and-planetary-sciences\/quartz-vein\">quartz veins<\/a> implied the development of an intense sericitization, most evident in the CA; (V) circulation of later hot fluids implied alteration and concentration of metallic phases.<\/p>\n<\/div>\n<p>Read the full article <a href=\"https:\/\/doi.org\/10.1016\/j.jsg.2019.04.009\">here<\/a>.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Gon\u00e7alves, A., Sant\u2019Ovaia, H., Noronha, F., 2019.\u00a0Emplacement mechanism of Caria-Vila da Ponte Pluton (Northern Portugal): Building and internal magmatic record. J Struc Geol 124, 91-111. The late to post-tectonic biotite granites from Caria\u2013Vila da Ponte area were studied for their mineralogical, microstructural and petrophysical standpoint using anisotropy of magnetic susceptibility coupled to petrography and scanning [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[16],"tags":[132,131,128,136,134,130,135,129,133],"_links":{"self":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts\/1605"}],"collection":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/comments?post=1605"}],"version-history":[{"count":2,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts\/1605\/revisions"}],"predecessor-version":[{"id":1607,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts\/1605\/revisions\/1607"}],"wp:attachment":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/media?parent=1605"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/categories?post=1605"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/tags?post=1605"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}