ºÝºÝߣshows by User: CHARLESKOMADJA / http://www.slideshare.net/images/logo.gif ºÝºÝߣshows by User: CHARLESKOMADJA / Tue, 24 Jul 2018 15:38:04 GMT ºÝºÝߣShare feed for ºÝºÝߣshows by User: CHARLESKOMADJA Rocks & usages /slideshow/rocks-usages/107309647 rocksusages-180724153804
Types of rocks and their potential use]]>
Types of rocks and their potential use]]> Tue, 24 Jul 2018 15:38:04 GMT /slideshow/rocks-usages/107309647 CHARLESKOMADJA@slideshare.net(CHARLESKOMADJA) Rocks & usages CHARLESKOMADJA Types of rocks and their potential use <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/rocksusages-180724153804-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> Types of rocks and their potential use
Rocks & usages from CHARLESKOMADJA
]]> 24 2 https://cdn.slidesharecdn.com/ss_thumbnails/rocksusages-180724153804-thumbnail.jpg?width=120&height=120&fit=bounds presentation Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 Mise en place de magmas ant¨¦ et syn-tectoniques dans le complexe intrusif de Wari-Maro dans la zone de cisaillement de Kandi, Centre-B¨¦nin, Afrique de l¡¯Ouest https://fr.slideshare.net/slideshow/mise-en-place-de-magmas-ant-et-syntectoniques-dans-le-complexe-intrusif-de-warimaro-dans-la-zone-de-cisaillement-de-kandi-centrebnin-afrique-de-louest/107306576 komadjaetal2017wari-maro-180724151543
The Wari-Maro intrusive complex is formed by meta-monzosyenites, monzogranites and diorite quartzifere setting up during the Neoproterozoic orogeny. The facies of this complex originate from the crystallization of pre-and syn-tectonic magmas relative to the deformation in the Kandi shear zone. The monzogranites are pre-tectonic. They are deformed and transformed into meta-monzosyenites under amphibolite facies metamorphic conditions during the dextral shearing. The garnet-monzogranites show a magmatic flow fabric suggesting magma emplacement and crystallization under shear strain. The diorite quartzifere is emplaced during late-tectonic phase in the Wari-Maro massif. The Wari-Maro complex offers a good opportunity to study the relationship between deformation and magmatism in the late-orogenic major shear zones of the Dahom¨¦yides fold belt.]]>
The Wari-Maro intrusive complex is formed by meta-monzosyenites, monzogranites and diorite quartzifere setting up during the Neoproterozoic orogeny. The facies of this complex originate from the crystallization of pre-and syn-tectonic magmas relative to the deformation in the Kandi shear zone. The monzogranites are pre-tectonic. They are deformed and transformed into meta-monzosyenites under amphibolite facies metamorphic conditions during the dextral shearing. The garnet-monzogranites show a magmatic flow fabric suggesting magma emplacement and crystallization under shear strain. The diorite quartzifere is emplaced during late-tectonic phase in the Wari-Maro massif. The Wari-Maro complex offers a good opportunity to study the relationship between deformation and magmatism in the late-orogenic major shear zones of the Dahom¨¦yides fold belt.]]> Tue, 24 Jul 2018 15:15:42 GMT https://fr.slideshare.net/slideshow/mise-en-place-de-magmas-ant-et-syntectoniques-dans-le-complexe-intrusif-de-warimaro-dans-la-zone-de-cisaillement-de-kandi-centrebnin-afrique-de-louest/107306576 CHARLESKOMADJA@slideshare.net(CHARLESKOMADJA) Mise en place de magmas ant¨¦ et syn-tectoniques dans le complexe intrusif de Wari-Maro dans la zone de cisaillement de Kandi, Centre-B¨¦nin, Afrique de l¡¯Ouest CHARLESKOMADJA The Wari-Maro intrusive complex is formed by meta-monzosyenites, monzogranites and diorite quartzifere setting up during the Neoproterozoic orogeny. The facies of this complex originate from the crystallization of pre-and syn-tectonic magmas relative to the deformation in the Kandi shear zone. The monzogranites are pre-tectonic. They are deformed and transformed into meta-monzosyenites under amphibolite facies metamorphic conditions during the dextral shearing. The garnet-monzogranites show a magmatic flow fabric suggesting magma emplacement and crystallization under shear strain. The diorite quartzifere is emplaced during late-tectonic phase in the Wari-Maro massif. The Wari-Maro complex offers a good opportunity to study the relationship between deformation and magmatism in the late-orogenic major shear zones of the Dahom¨¦yides fold belt. <img style="border:1px solid #C3E6D8;float:right;" alt="" src="https://cdn.slidesharecdn.com/ss_thumbnails/komadjaetal2017wari-maro-180724151543-thumbnail.jpg?width=120&amp;height=120&amp;fit=bounds" /><br> The Wari-Maro intrusive complex is formed by meta-monzosyenites, monzogranites and diorite quartzifere setting up during the Neoproterozoic orogeny. The facies of this complex originate from the crystallization of pre-and syn-tectonic magmas relative to the deformation in the Kandi shear zone. The monzogranites are pre-tectonic. They are deformed and transformed into meta-monzosyenites under amphibolite facies metamorphic conditions during the dextral shearing. The garnet-monzogranites show a magmatic flow fabric suggesting magma emplacement and crystallization under shear strain. The diorite quartzifere is emplaced during late-tectonic phase in the Wari-Maro massif. The Wari-Maro complex offers a good opportunity to study the relationship between deformation and magmatism in the late-orogenic major shear zones of the Dahom¨¦yides fold belt.
from CHARLESKOMADJA
]]> 86 2 https://cdn.slidesharecdn.com/ss_thumbnails/komadjaetal2017wari-maro-180724151543-thumbnail.jpg?width=120&height=120&fit=bounds document Black http://activitystrea.ms/schema/1.0/post http://activitystrea.ms/schema/1.0/posted 0 https://public.slidesharecdn.com/v2/images/profile-picture.png https://cdn.slidesharecdn.com/ss_thumbnails/rocksusages-180724153804-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/rocks-usages/107309647 Rocks &amp; usages https://cdn.slidesharecdn.com/ss_thumbnails/komadjaetal2017wari-maro-180724151543-thumbnail.jpg?width=320&height=320&fit=bounds slideshow/mise-en-place-de-magmas-ant-et-syntectoniques-dans-le-complexe-intrusif-de-warimaro-dans-la-zone-de-cisaillement-de-kandi-centrebnin-afrique-de-louest/107306576 Mise en place de magma...