{"id":922,"date":"2018-04-17T23:45:43","date_gmt":"2018-04-17T22:45:43","guid":{"rendered":"https:\/\/engel-bergbau.de\/?page_id=922"},"modified":"2025-11-27T15:10:56","modified_gmt":"2025-11-27T14:10:56","slug":"geologie","status":"publish","type":"page","link":"https:\/\/engel-bergbau.de\/fr\/bergbau\/geologie\/","title":{"rendered":"G\u00e9ologie"},"content":{"rendered":"

[et_pb_section fb_built=“1″ admin_label=“header_bergbau“ _builder_version=“4.16″ background_color=“#e2d4c0″ background_image=“https:\/\/engel-bergbau.de\/wp-content\/uploads\/2018\/04\/Luftbild-Abtransport-2018-02-19-um-17.11.24.png“ custom_margin=“|||“ custom_padding=“10%|0px|10%|0px“ global_colors_info=“{}“][\/et_pb_section][et_pb_section fb_built=“1″ _builder_version=“4.16″ global_colors_info=“{}“][et_pb_row _builder_version=“4.16″ max_width=“842px“ module_alignment=“center“ custom_margin=“|||“ custom_padding=“100px|||“ use_custom_width=“on“ custom_width_px=“842px“ global_colors_info=“{}“][et_pb_column type=“4_4″ _builder_version=“4.16″ custom_padding=“|||“ global_colors_info=“{}“ custom_padding__hover=“|||“][et_pb_text admin_label=“Tittle“ _builder_version=“4.16″ text_font=“Nunito||||||||“ text_font_size=“18px“ text_line_height=“1.8em“ header_font=“||||||||“ header_text_align=“center“ header_3_font=“Oswald|||on|||||“ header_3_font_size=“42px“ header_3_letter_spacing=“2px“ header_3_line_height=“1.5em“ max_width=“600%“ max_width_tablet=““ max_width_phone=““ max_width_last_edited=“on|phone“ module_alignment=“left“ custom_margin=“|||“ locked=“off“ global_colors_info=“{}“]<\/p>\n

G\u00e9ologie<\/h3>\n

\u00a0La mine de gypse \/ d\u2019anhydrite \u00ab\u00a0Horst-Peter-Stollen\u00a0\u00bb se situe dans une formation g\u00e9ologique appel\u00e9e \u00ab\u00a0bassin triasique de Tr\u00eaves-Bitburg\u00a0\u00bb. Ce dernier renferme des d\u00e9p\u00f4ts triasiques datant d\u2019il y a 253 \u00e0 202\u00a0millions d\u2019ann\u00e9es faisant eux-m\u00eames partie d\u2019un plus grand ensemble, le \u00ab\u00a0bassin germanique\u00a0\u00bb. Le bassin triasique de Tr\u00eaves-Bitburg se trouve, quant \u00e0 lui, entre le massif rh\u00e9nan et le massif du Brabant.<\/span><\/p>\n

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La coupe g\u00e9ologique ci-dessous illustre la localisation pr\u00e9cise de la mine ainsi que les principaux \u00e9l\u00e9ments g\u00e9ologiques du bassin triasique de Tr\u00eaves-Bitburg. Le gisement de gypse se situe dans la roche compos\u00e9e de falun (datant d\u2019il y a 246 \u00e0 239 millions d\u2019ann\u00e9es).<\/p>\n

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Le gisement actuellement exploit\u00e9 a une \u00e9paisseur d\u2019environ 10\u00a0m\u00e8tres. Le gypse fait partie des roches dites \u00ab\u00a0\u00e9vaporites\u00a0\u00bb.\u00a0Dans une lagune, par exemple, la concentration des min\u00e9raux augmente par \u00e9vaporation de l\u2019eau de mer.\u00a0Si la concentration d\u00e9passe un certain seuil, il y a pr\u00e9cipitation de gypse (CaSO4 <\/span>* 2 H2<\/span>O). \u00c0 la suite de ce processus appel\u00e9 \u00ab\u00a0diag\u00e9n\u00e8se\u00a0\u00bb l\u2019eau est chass\u00e9e, le gypse se transforme en anhydrite (CaSO4<\/span>), ou autrement dit en gypse d\u00e9shydrat\u00e9. Plus tard, si les conditions requises sont r\u00e9unies, cette r\u00e9action s\u2019inverse\u00a0: une partie ou l\u2019int\u00e9gralit\u00e9 de l\u2019anhydrite se transforme \u00e0 nouveau en gypse.<\/p>\n

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Nos bureaux<\/span><\/h2>\n

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Gipsbergbau ENGEL GmbH
Auf der Hill 6 a
54295 Trier, Allemagne
T\u00e9l.\u00a0: +49 651 33131
Fax\u00a0: +49 651 308361
info@engel-bergbau.de<\/a><\/p>\n

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Production<\/span><\/h2>\n

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Gipsbergbau ENGEL GmbH
\u00ab\u00a0Horst-Peter-Stollen\u00a0\u00bb
Zur Gipsgrube 1
54310 Ralingen, Allemagne
T\u00e9l.\u00a0: +49 6585 839
Fax\u00a0: +49 6585 991218
produktion@engel-bergbau.de<\/a><\/p>\n

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Liens<\/span><\/h2>\n

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Protection des donn\u00e9es<\/a><\/p>\n

Mentions l\u00e9gales<\/a><\/p>\n

Plan d'acc\u00e8s<\/a><\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>","protected":false},"excerpt":{"rendered":"

Geologie \u00a0Das Gips-Anhydrit Bergwerk \u201eHorst Peter-Stollen\u201c liegt in einer geologischen Baueinheit, die als \u201eTrier-Bitburger-Triasmulde\u201c\u00a0bezeichnet wird. Die Ablagerungen der Trias (vor ca. 253 bis 202 Mio. Jahren) in diesem Bereich geh\u00f6rten wiederum\u00a0zu der Gro\u00dfeinheit des Germanischen Beckens. Die \u201eTrier-Bitburger-Triasmulde\u201c ist zwischen den Festl\u00e4ndern \u201eRheinischem\u00a0Massiv\u201c und \u201eBrabanter Massiv\u201c zu lokalisieren.Der geologische Schnitt durch die \u201eTrier-Bitburger-Triasmulde\u201c zeigt die […]<\/p>","protected":false},"author":2,"featured_media":0,"parent":17,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-922","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/pages\/922","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/comments?post=922"}],"version-history":[{"count":19,"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/pages\/922\/revisions"}],"predecessor-version":[{"id":1642,"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/pages\/922\/revisions\/1642"}],"up":[{"embeddable":true,"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/pages\/17"}],"wp:attachment":[{"href":"https:\/\/engel-bergbau.de\/fr\/wp-json\/wp\/v2\/media?parent=922"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}