Metamorphic map of the Alps<\/p>\n
From Corsica to the Vienna basin (Austria), the Metamorphic map of the Alps<\/em> offers a compilation, at the millionth scale, of the different metamorphic conditions recorded during the Alpine orogeny since the Cretaceous. This synthesis is both an update and a reworking of the \"Map of the metamorphic structure of the Alps\".<\/em> published in 2004 by Oberh\u00e4nsli et al<\/em>. Associated with the main map, a set of additional documents provides complementary data : Metamorphic map of the Alps<\/p>\n The completion of this work, as well as the Tectonic map of the Alps (2012),<\/em> is part of a general synthesis of geological, petrological and geophysical data acquired in the Alps. By favouring this approach, it remains representative of the state of knowledge at a given moment, a state which leaves many questions open and which therefore constitutes only a fundamental element of future discussions. In this perspective, and following the example of the map published in 2004, the Metamorphic map of the Alps<\/em> proposes a global approach to the chain and attempts to account for the geodynamic evolution over time.<\/p>\n For more information on this map see http:\/\/www.geodynalps.eu<\/p>","protected":false},"excerpt":{"rendered":" Metamorphic map of the Alps<\/p>\n Scale: 1:1 000 000 Map also available in digital pdf version on our catalogue and in folded paper version.<\/p>","protected":false},"featured_media":10305,"comment_status":"closed","ping_status":"closed","template":"","meta":{"inline_featured_image":false,"site-sidebar-layout":"default","site-content-layout":"default","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"default","adv-header-id-meta":"","stick-header-meta":"default","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"set","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}}},"product_cat":[59,54,62,68,61],"product_tag":[488,489,490],"_links":{"self":[{"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/product\/9103"}],"collection":[{"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/product"}],"about":[{"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/types\/product"}],"replies":[{"embeddable":true,"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/comments?post=9103"}],"version-history":[{"count":0,"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/product\/9103\/revisions"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/media\/10305"}],"wp:attachment":[{"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/media?parent=9103"}],"wp:term":[{"taxonomy":"product_cat","embeddable":true,"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/product_cat?post=9103"},{"taxonomy":"product_tag","embeddable":true,"href":"https:\/\/ccgm.org\/en\/wp-json\/wp\/v2\/product_tag?post=9103"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}
\n- on the different stages of the construction of the Alpine chain by a map of the tectonic-metamorphic age distributions on a scale of 1 : 2 500 000;
\n- on the depth distribution of metamorphic units along the four Alpine seismic profiles (TRANSALP, NFP20 East, NFP20 West, ECORS-CROP)
\n- on the interpretations, in terms of tectonic-metamorphic ages, of these four seismic profiles
\n- on the metamorphic facies recognised in the Alps, and the description of the different mineralogical associations according to the chemistry of the rocks.<\/p>\n
\nPublished in November 2012
\nSize: 124 x 100 cm
\nEquidistant conical projection
\nCCGM-CGMW 2012
\nAuthors: Romain Bousquet, Stefan M. Schmid, Gerold Zeilinger, Roland Oberh\u00e4nsli, Claudio Rosenberg, Giancarlo Molli, Christian Robert, Michael Wiederkehr, Friedrich Koller and Andreas M\u00f6ller<\/p>\n