{"id":5109,"date":"2023-03-13T12:16:00","date_gmt":"2023-03-13T12:16:00","guid":{"rendered":"https:\/\/www.icterra.pt\/?page_id=5109"},"modified":"2023-03-13T12:16:00","modified_gmt":"2023-03-13T12:16:00","slug":"special-issue-petrographic-geophysical-geochemical-and-geochronological-study-of-magma-and-magmatism-in-the-iberian-peninsula-and-archipelagos","status":"publish","type":"page","link":"https:\/\/www.icterra.pt\/legacy\/index.php\/special-issue-petrographic-geophysical-geochemical-and-geochronological-study-of-magma-and-magmatism-in-the-iberian-peninsula-and-archipelagos\/","title":{"rendered":"Special Issue “Petrographic, Geophysical, Geochemical and Geochronological Study of Magma and Magmatism in the Iberian Peninsula and Archipelagos”"},"content":{"rendered":"

Magmatism is the most important process for crustal growth and differentiation. Mantle or crustal decompression, volatile addition and heat-induced melting, on astenospheric and lithospheric scale, are essential mechanisms involved in the origin of primary partial melts, although fractional crystallisation, magma mixing and assimilation also play a significant role in their evolution. In many cases, magmatism favours ore-forming conditions and promotes the generation of profitable mineral deposits. The spatio-temporal and geophysico-chemical evolution of magmas is crucial to understand the nature of the mantle and\/or crustal sources and the magmatic processes operating during melt extraction, magma ascent and their final emplacement, usually reflected in the mineral paragenesis, texture, structure and geochemical and isotopic features of igneous materials.<\/span><\/p>\n

Igneous lithologies of distinct geochemical affinity (calc-alkaline, alkaline, tholeiitic and shoshonitic) and geophysical signature are widely distributed in the Iberian Peninsula, associated to diverse tectono-thermal episodes from Late Neoproterozoic to Late-Palaeozoic, Mesozoic and Cenozoic times. Magmatic rocks form a major component in western Iberia, although they are also profuse in its northeastern and southeastern edges. They are a fundamental constituent of the Spanish-Portuguese archipelagos. Critical elements mineralisations are usually related to these lithologies.<\/span><\/p>\n

This Special Issue is intended to improve our knowledge regarding the processes involved in the generation and evolution of magmatism in the Iberian Peninsula and the Spanish-Portuguese archipelagos, contributing to a better understanding of transport and emplacement mechanisms, as well as the mineralization patterns in magmatic systems.<\/span><\/p>\n

Dr. Enrique Merino Mart\u00ednez<\/span>
\nDr. David Orejana Garc\u00eda<\/span>
\nDr. Helena Sant\u2019Ovaia<\/span>
\nGuest Editors<\/em><\/span><\/p>\n

Manuscript Submission Information<\/strong><\/span><\/p>\n

Manuscripts should be submitted online at\u00a0www.mdpi.com<\/a>\u00a0by\u00a0registering<\/a>\u00a0and\u00a0logging in to this website<\/a>. Once you are registered,\u00a0click here to go to the submission form<\/a>. Manuscripts can be submitted until the deadline. All submissions that pass pre-check are peer-reviewed. Accepted papers will be published continuously in the journal (as soon as accepted) and will be listed together on the special issue website. Research articles, review articles as well as short communications are invited. For planned papers, a title and short abstract (about 100 words) can be sent to the Editorial Office for announcement on this website.<\/span><\/p>\n

Submitted manuscripts should not have been published previously, nor be under consideration for publication elsewhere (except conference proceedings papers). All manuscripts are thoroughly refereed through a single-blind peer-review process. A guide for authors and other relevant information for submission of manuscripts is available on the\u00a0Instructions for Authors<\/a>\u00a0page.\u00a0Minerals<\/em><\/a>\u00a0is an international peer-reviewed open access monthly journal published by MDPI.<\/span><\/p>\n

Please visit the\u00a0Instructions for Authors<\/a>\u00a0page before submitting a manuscript. The\u00a0Article Processing Charge (APC)<\/a>\u00a0for publication in this\u00a0open access<\/a>\u00a0journal is 2000 CHF (Swiss Francs). Submitted papers should be well formatted and use good English. Authors may use MDPI’s\u00a0English editing service<\/a>\u00a0prior to publication or during author revisions.<\/span><\/p>\n

https:\/\/www.mdpi.com\/journal\/minerals\/special_issues\/WC14HH132K<\/span><\/p>\n

Flyer<\/span><\/a><\/p>\n","protected":false},"excerpt":{"rendered":"

Magmatism is the most important process for crustal growth and differentiation. Mantle or crustal decompression, volatile addition and heat-induced melting, on astenospheric and lithospheric scale, are essential mechanisms involved in the origin of primary partial melts, although fractional crystallisation, magma mixing and assimilation also play a significant role in their evolution. In many cases, magmatism […]<\/p>\n","protected":false},"author":3,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"_links":{"self":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/pages\/5109"}],"collection":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/types\/page"}],"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=5109"}],"version-history":[{"count":1,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/pages\/5109\/revisions"}],"predecessor-version":[{"id":5111,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/pages\/5109\/revisions\/5111"}],"wp:attachment":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/media?parent=5109"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}