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Detail aus dem Glasmosaik &bdquo;Reichtum Erde&ldquo; von Christian Ludwig Attersee im Foyer der Geologischen Bundesanstalt. &copy; Geosphere Austria
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</figcaption></figure></div></div></div></div></div><div class="ce-bodytext"><h2>Geologie kurz und bunt</h2><p>Die Fragen nach der Entstehung des Bodens unter unseren F&uuml;&szlig;en, also nach Art, Herkunft und Alter der Gesteine und der Geschichte der Formung der Landschaft, z&auml;hlen seit jeher zu den nat&uuml;rlichen Grundfragen des Menschen.
</p><p>Antworten werden auf mythologischer, philosophischer und theologischer Ebene zu geben versucht. Rocky Austria stellt die geologische Entwicklung unseres Landes, basierend auf naturwissenschaftlichen Daten, dar. Deren Erforschung war und ist h&auml;ufig von praktischen Interessen motiviert, wie der Suche nach nutzbaren Vorkommen von mineralischen Rohstoffen oder der Versorgung mit sauberem Trinkwasser. Aber auch ein kulturelles Bed&uuml;rfnis vieler ist damit verbunden: Herkunft und Werden der Gesteine und Landschaften sollen auf aktuellem wissenschaftlichem Kenntnisstand verst&auml;ndlich erl&auml;utert werden!</p></div></div></div></div>
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Glossar
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Begriffe von A - Z
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<div id="c12904" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="../glossar.html" title="Im selben Fenster: Glossar Buchstabe A" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>A</b></a></td><td><a href="glossar-b.html" title="Im selben Fenster: Glossar Buchstabe B" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>B</b></a></td><td><a href="glossar-c.html" title="Im selben Fenster: Glossar Buchstabe C" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>C</b></a></td><td><a href="glossar-d.html" title="Im selben Fenster: Glossar Buchstabe D" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>D</b></a></td><td><a href="glossar-e.html" title="Im selben Fenster: Glossar Buchstabe E" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>E</b></a></td><td><a href="glossar-f.html" title="Im selben Fenster: Glossar Buchstabe F" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>F</b></a></td><td><a href="glossar-g.html" title="Im selben Fenster: Glossar Buchstabe G" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>G</b></a></td><td><a href="glossar-h.html" title="Im selben Fenster: Glossar Buchstabe H" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>H</b></a></td><td><a href="glossar-i.html" title="Im selben Fenster: Glossar Buchstabe I" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>I</b></a></td><td><a href="glossar-k.html" title="Im selben Fenster: Glossar Buchstabe K" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>K</b></a></td><td><a href="glossar-l.html" title="Im selben Fenster: Glossar Buchstabe L" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>L</b></a></td></tr></tbody></table><table style="BORDER-TOP-COLOR: #dddddd; BORDER-BOTTOM-COLOR: #dddddd; BORDER-RIGHT-COLOR: #dddddd; BORDER-LEFT-COLOR: #dddddd" class="contenttable"><tbody><tr><td><a href="glossar-m.html" title="Im selben Fenster: Glossar Buchstabe M" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>M</b></a></td><td><a href="glossar-n.html" title="Im selben Fenster: Glossar Buchstabe N" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>N</b></a></td><td rowspan="1"><a href="glossar-o.html" title="Im selben Fenster: Glossar Buchstabe O" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>O</b></a></td><td rowspan="1"><a href="glossar-p.html" title="Im selben Fenster: Glossar Buchstabe P" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>P</b></a></td><td rowspan="1"><a href="glossar-q.html" title="Im selben Fenster: Glossar Buchstabe Q" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>Q</b></a></td><td rowspan="1"><a href="glossar-r.html" title="Im selben Fenster: Glossar Buchstabe R" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>R</b></a></td><td rowspan="1"><b>S</b></td><td rowspan="1"><a href="glossar-t.html" title="Im selben Fenster: Glossar Buchstabe T" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>T</b></a></td><td rowspan="1"><a href="glossar-u.html" title="Im selben Fenster: Glossar Buchstabe U" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>U</b></a></td><td rowspan="1"><a href="glossar-v.html" title="Im selben Fenster: Glossar Buchstabe V" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>V</b></a></td><td rowspan="1"><a href="glossar-z.html" title="Im selben Fenster: Glossar Buchstabe Z" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span><b>Z</b></a></td></tr></tbody></table></div>
<div id="c12474" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sand:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment</a> im Korngr&ouml;&szlig;enbereich von 0,063 mm bis 2 mm.</p></div>
<div id="c12711" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sandstein:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sedimentgestein</a> im Korngr&ouml;&szlig;enbereich von 0,063 mm bis 2 mm.</p></div>
<div id="c12712" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Saures Gestein:</h3><p><a href="glossar-m.html#c12655" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Magmatisches Gestein</a> mit einem hohen SiO<sub>2</sub>-Gehalt von mehr als 63 %.</p></div>
<div id="c12713" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schelf:</h3><p>Randbereich der Kontinente, der bis ca. 200 m Wassertiefe unter dem Meeresspiegel liegt.</p></div>
<div id="c12714" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schelfmeer:</h3><p>Flachwasserbereich am <a href="glossar-s.html#c12713" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Schelf</a>.</p></div>
<div id="c12715" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schichtflut:</h3><p>Fl&auml;chenhafter, schlammbeladener Wasserabfluss auf leicht geneigter Ebene.</p></div>
<div id="c12716" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schichtl&uuml;cke:</h3><p><a href="glossar-s.html#c13190" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Stratigraphische</a> L&uuml;cke innerhalb einer durchgehenden Ablagerung von <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment</a>, hervorgerufen durch Unterbrechung der <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment</a>ation und eventuell zus&auml;tzlich <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Erosion</a>.</p></div>
<div id="c13189" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schichtfolge:</h3><p>Bezeichnung f&uuml;r kontinuierlich &uuml;bereinander abgelagerte <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gestein</a>sschichten, die eine Entwicklungsgeschichte erz&auml;hlen, z. B. von Seicht- zu Tiefwasserablagerungen.</p></div>
<div id="c12717" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schiefer:</h3><p><a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gestein</a> mit einer schiefrigen Struktur und einer Spaltbarkeit von unter 1 cm. Der Gehalt an <a href="glossar-f.html#c12589" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Feldspat</a> liegt unter 20 % und ein Lagenbau ist gew&ouml;hnlich vorhanden.</p></div>
<div id="c12718" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schieferton:</h3><p>Geschichtetes <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sedimentgestein</a> mit einer Korngr&ouml;&szlig;e &lt; 0.002 mm.</p></div>
<div id="c12719" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schlier:</h3><p>Informelle Bezeichnung f&uuml;r fein<a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>sandig</a>-schluffigen (<a href="glossar-s.html#c12720" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Schluff</a>) Mergel im Bereich der <a href="glossar-m.html#c12670" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Molasse</a>zone und des Steirischen Beckens.</p></div>
<div id="c12720" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schluff:</h3><p>Alternativer Name f&uuml;r <a href="glossar-s.html#c12731" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Silt</a>.</p></div>
<div id="c12721" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schotter:</h3><p>Besteht haupts&auml;chlich aus <a href="glossar-k.html#c12631" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Kies</a>.</p></div>
<div id="c12722" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Schuppe:</h3><p>Subeinheit einer <a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Decke</a>.</p></div>
<div id="c12723" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sediment:</h3><p>Entsteht durch Ablagerung von <a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>klastischem</a> Material, das durch Luft, Wasser, Eis, Wind transportiert wird, oder aus Material, welches sich durch chemische F&auml;llung aus L&ouml;sung bzw. aus Abscheidung durch Organismen bildet. Formt lockere, nicht konsolidierte Lagen und K&ouml;rper an der Erdoberfl&auml;che.</p></div>
<div id="c12724" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sedimentgestein:</h3><p>Verfestigtes <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment</a>, welches durch Entw&auml;sserung, Volumenverkleinerung, Zementbildung oder biogene Verkittung entsteht (<a href="glossar-d.html#c12572" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Diagenese</a>).</p></div>
<div id="c12725" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Seife:</h3><p>&Ouml;rtliche Anh&auml;ufung von spezifisch schweren <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Mineralen</a> in <a href="glossar-s.html#c12474" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sand </a>oder <a href="glossar-k.html#c12631" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Kies</a>.</p></div>
<div id="c12726" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Seitenverschiebung:</h3><p>Eine steil stehende bis vertikale <a href="glossar-s.html#c12734" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>St&ouml;rung</a> mit &uuml;berwiegend horizontaler Verschiebung der angrenzenden <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gesteins</a>k&ouml;rper.</p></div>
<div id="c12727" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Serpentin-Gruppe:</h3><p>Feinbl&auml;ttrige, sehr magnesiumreiche Schicht<a href="glossar-s.html#c12729" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>silikate</a>.</p></div>
<div id="c12728" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Serpentinit:</h3><p>Gr&uuml;nes bis schwarzes <a href="glossar-m.html#c12663" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>metamorphes</a><a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gestein</a>, welches vornehmlich aus <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Mineralen</a> der <a href="glossar-s.html#c12727" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Serpentin-Gruppe</a> besteht, gebildet durch Wasseraufnahme von <a href="glossar-u.html#c12750" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Ultrabasit</a>.</p></div>
<div id="c12730" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Sibiria:</h3><p>Ehemaliger proterozoischer bis pal&auml;ozoischer Kontinent, der im Perm im Zuge der <a href="glossar-g.html#c12598" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gebirgsbildung</a> des Ural dem Gro&szlig;kontinent <a href="glossar-p.html#c12683" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Pang&auml;a</a> angegliedert wurde.</p></div>
<div id="c12729" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Silikate:</h3><p>Salze verschiedener <a href="glossar-k.html#c12634" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Kiesels&auml;uren</a>; einfache Silikat-Ionen bestehen aus SiO<sub>4</sub>-Tetraedern, die zu verschiedenen Strukturen wie beispielsweise Ketten-, Schicht- oder Ger&uuml;stsilikaten verkn&uuml;pft sind. Nat&uuml;rliche Silikate spielen eine gro&szlig;e Rolle in der <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Geologie</a>, da sehr viele <a href="glossar-m.html#c12666" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Minerale</a> dieser Stoffgruppe angeh&ouml;ren. Die <a href="glossar-e.html#c12583" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Erdkruste</a> besteht zu &uuml;ber 90 Prozent, der <a href="glossar-e.html#c12584" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Erdmantel</a> fast vollst&auml;ndig aus Silikaten.</p></div>
<div id="c12731" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Silt:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Klastisches</a><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment</a> im Korngr&ouml;&szlig;enbereich zwischen 0,002 und 0,063 mm, auch als <a href="glossar-s.html#c12720" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Schluff</a> bezeichnet.</p></div>
<div id="c12732" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Siltstein:</h3><p><a href="glossar-k.html#c12757" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Klastisches</a><a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sedimentgestein</a> im Korngr&ouml;&szlig;enbereich zwischen 0,002 und 0,063 mm.</p></div>
<div id="c13226" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Spurenfossilien:</h3><p>Hinweise in <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sedimenten</a> auf Vorkommen, Lebensumst&auml;nde und Verhalten <a href="glossar-f.html#c12595" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>fossiler</a> Organismen zu Lebzeiten.</p></div>
<div id="c12733" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Steinsalz:</h3><p>Chemisches <a href="glossar-s.html#c12724" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sedimentgestein</a>, das zu mehr als der H&auml;lfte aus grob <a href="glossar-k.html#c12645" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>kristallinem</a> Salz (Natriumchlorid) besteht, typischerweise durch Eisenoxide gef&auml;rbt und mit <a href="glossar-t.html#c12743" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Ton</a> vermischt.</p></div>
<div id="c13190" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Stratigraphie:</h3><p>Teilgebiet der Historischen Geologie, das die zeitliche und r&auml;umliche Ordnung der Gesteine unter Ber&uuml;cksichtigung aller physikalischen und chemischen Grundmerkmale (Fossilinhalt, Zusammensetzung etc.) zum Ziel hat. Sie ist somit Basis und Ma&szlig;stab f&uuml;r die Kl&auml;rung und Parallelisierung erdgeschichtlicher und regionalgeologischer Prozesse.</p></div>
<div id="c12734" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>St&ouml;rung:</h3><p>Grenzfl&auml;che, die zwei <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gesteins</a>einheiten trennt und an der Bewegung stattgefunden hat.</p></div>
<div id="c13225" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Str&ouml;mungsmarken:</h3><p><a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment&auml;re</a><a href="glossar-s.html#c12735" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Strukturen</a>, die als <a href="glossar-e.html#c12585" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Erosions</a>formen auf <a href="glossar-s.html#c12723" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Sediment</a>oberfl&auml;chen durch dar&uuml;ber str&ouml;mendes Wasser entstehen.</p></div>
<div id="c12735" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Struktur:</h3><p>In der <a href="glossar-g.html#c12601" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Geologie</a> die generelle Anordnung von <a href="glossar-g.html#c12603" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gesteins</a>massen, insbesondere Lage, Gef&uuml;ge (<a href="glossar-g.html#c12599" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Gef&uuml;gekunde</a>) oder relative Position in einem Gebiet oder einer Region.</p></div>
<div id="c12736" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-standard"><h3>Subduktion:</h3><p>Abtauchen einer Lithosph&auml;renplatte (<a href="glossar-l.html#c12652" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Lithosph&auml;re</a>) unter eine andere.</p></div>
<div id="c13223" class="frame frame-default frame-type-text frame-layout-0 frame-space-before-standard frame-space-after-custom-5"><h3>Subpenninikum:</h3><p>Bezeichnung f&uuml;r die <a href="glossar-t.html#c12738" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>tektonische</a> Lage dieser Einheit unter den <a href="glossar-p.html#c12687" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Penninischen</a><a href="glossar-d.html#c12390" title="Opens internal link in current window" class="internal-link"><span class="link-prefix">&raquo;&nbsp;</span>Decken</a>, also in &bdquo;sub&ldquo;penninischer Position.</p></div>
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