{"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\/en\/bergbau\/geologie\/","title":{"rendered":"Geology"},"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

Geology<\/h3>\n

\u00a0The Horst-Peter-Stollen gypsum-anhydrite mine is in a geological formation called the \u201cTrier-Bitburger Triassic Syncline\u201d. The Triassic deposits found here (dating back 253-202 million years) are part of the larger Germanic Basin. The syncline is situated between the Rhenish and London-Brabant Massifs.\nThe geological cross-section below shows the exact location of the mine and the most significant geological features of the Trier-Bitburger Triassic Syncline. The gypsum deposit is in the Muschelkalk rock layer (Muschelkalk dating back 246-239 million years).<\/span><\/p>\n

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The geological cross-section below shows the exact location of the mine and the most significant geological features of the Trier-Bitburger Triassic Syncline. The gypsum deposit is in the Muschelkalk rock layer (Muschelkalk dating back 246-239 million years).<\/p>\n

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The deposit that is currently being worked is about ten metres thick. Gypsum is a so-called evaporite rock. When seawater gets trapped in a restricted basin and begins to evaporate, it becomes more concentrated and enriched in minerals. Over a certain level of concentration, the minerals precipitate to form gypsum (CaSO4 * 2 H2O). As this diagenesis continues, the water evaporates completely, forming anhydrite (CaSO4) or, in other words, \u201cwater-free gypsum\u201d. Later, in the right conditions, anhydrite can partly or fully turn back into gypsum.<\/p>\n

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Our offices<\/span><\/h2>\n

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Gips Bergbau ENGEL GmbH
Auf der Hill 6 a
54295 Trier, Germany
Phone: +49 651 33131
Fax: +49 651 308361
info@engel-bergbau.de<\/a><\/p>\n

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

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Gips Bergbau ENGEL GmbH
Horst-Peter-Stollen
Zur Gipsgrube 1
54310 Ralingen,\nGermany
Phone: +49 6585 839
Fax: +49 6585 991218
produktion@engel-bergbau.de<\/a><\/p>\n

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Links<\/span><\/h2>\n

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Legal notice<\/a><\/p>\n

Approach<\/a><\/p>\n

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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\/en\/wp-json\/wp\/v2\/pages\/922","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/comments?post=922"}],"version-history":[{"count":19,"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/pages\/922\/revisions"}],"predecessor-version":[{"id":1642,"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/pages\/922\/revisions\/1642"}],"up":[{"embeddable":true,"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/pages\/17"}],"wp:attachment":[{"href":"https:\/\/engel-bergbau.de\/en\/wp-json\/wp\/v2\/media?parent=922"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}