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In the central parts of the
Germanic Basin, the Germanic Trias has an average thickness of 800 meters, but regional differences are considerable. In the north of Germany the thickness of the Buntsandstein alone can exceed 1400 meters. The Germanic Trias lies on top of the
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has shown the age of the
Germanic Trias is not totally corresponding with the Triassic period. The base of the Buntsandstein was formed during the
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The base is not defined in the same way everywhere. In northern
Germany the base is formed by the
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means "threefold"). In the past the names of these three units were also used as units in the
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at least a few million years older than the
Triassic-Jurassic boundary. Usually there is a
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that covered much of midwestern Europe (including the south of the North Sea and
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In German lithostratigraphy, Buntsandstein, Muschelkalk and Keuper are seen as
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while the Dutch
Buntsandstein is subdivided in a number of formations. The
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lithostratigraphy divides the
Germanic Trias along other boundaries in a
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Ogg, James G.; Ogg, Gabi M.; Gradstein, Felix M. (2016). "Triassic".
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between the base of the Lias and top of the
Germanic Trias.
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Major lithostratigraphic units of northwest Europe with the
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536:. The Dutch Keuper and Muschelkalk have the status of
432:whereas the Buntsandstein and Keuper are mostly
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51:introducing citations to additional sources
544:of British stratigraphy is similar in age,
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41:Relevant discussion may be found on the
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413:The Germanic Trias formed in the large
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579:A Concise Geologic Time Scale: 2016
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548:and facies to the Buntsandstein.
397:, that gave the period its name (
34:relies largely or entirely on a
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581:. Elsevier. pp. 133–149.
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356:Germanische Trias-Supergruppe
624:Lithostratigraphy of Germany
502:. The top of the Keuper is
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534:Upper Germanic Trias Group
530:Lower Germanic Trias Group
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481:HeigenbrĂĽcken-Sandstone
16:Sequence of rock strata
495:of the Permian, about
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515:stratigraphic hiatus
506:in age and at about
362:unit (a sequence of
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479:by the base of the
456:units, such as the
619:Geology of Germany
558:Geology of Germany
485:Radiometric dating
403:geologic timescale
360:lithostratigraphic
588:978-0-444-63771-0
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36:single source
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292:251.2–251.9
282:247.2–251.2
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218:208.5–227.0
201:201.4–208.5
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434:continental
391:Muschelkalk
364:rock strata
247:Muschelkalk
603:Categories
564:References
538:formations
458:Lias Group
452:and below
423:Baltic Sea
374:) and the
165:Hettangian
133:Age (
73:newspapers
629:North Sea
546:lithology
471:, in the
376:North Sea
329:Zechstein
306:Lopingian
278:Olenekian
142:European
103:July 2024
43:talk page
552:See also
504:Rhaetian
477:Odenwald
473:Spessart
399:Triassic
380:Triassic
237:Ladinian
197:Rhaetian
188:Triassic
153:Jurassic
532:and an
447:Permian
358:) is a
299:Permian
254:Anisian
233:Middle
224:Carnian
172:younger
87:scholar
585:
542:Bunter
522:groups
430:facies
427:marine
409:Origin
395:Keuper
383:period
368:Europe
352:German
288:Induan
274:Lower
264:Bunter
214:Norian
207:Keuper
193:Upper
123:Series
118:System
89:
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526:Dutch
509:200.5
493:stage
419:basin
320:older
159:Lower
128:Stage
94:JSTOR
80:books
583:ISBN
475:and
417:, a
393:and
372:Alps
346:The
179:Lias
66:news
498:252
460:or
338:ICS
266:or
49:by
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135:Ma
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
