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The Wetterstein Formation is a regional ge … The Wetterstein Formation is a regional geologic formation of the Northern Limestone Alps and Western Carpathians extending from southern Bavaria, Germany in the west, through northern Austria to northern Hungary and western Slovakia in the east. The formation dates back to the Ladinian to Carnian stages of the Late Triassic. The formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians. The formation is composed of mostly reefal limestones and dolomites, the latter the result of widespread diagenesis. In many areas there is a frequent alternation of limestone and dolomite facies. Local variants to indicate the Wetterstein Formation include German: Wettersteinkalk (Wetterstein Limestone), Wettersteindolomit ("Wetterstein Dolomite") and combinations thereof. The Wetterstein Formation reaches a maximum thickness of 1,000 metres (3,300 ft) with major regional thickness variations. It belongs to the tectonostratigraphical unit Austroalpine nappes. The carbonate rock of the formation is from the Middle Triassic epoch of the Ladinian stage, comparable to the German stage in which Muschelkalk rock strata were formed. The formation has provided numerous fossils of corals, sponges, bivalves, gastropods and other marine groups indicative of a shallow marine carbonate platform environment deposited at the northern end of the Tethys Ocean.d at the northern end of the Tethys Ocean.
, Wettersteinský vápenec (německy Wettersteinkalk, anglicky Wetterstein Limestone) je pevný, zpravidla (světle) šedý vápenec, středně až svrchnětriasového stáří (ladin-spodní karn). Představuje horninu typickou pro jižnější jednotky Alp, Karpat a Dinarid.
, Wettersteinkalk und Wettersteindolomit sin … Wettersteinkalk und Wettersteindolomit sind die häufigsten Namen für ein Karbonatgestein aus der Mittleren Trias, der ladinischen Zeitstufe, vergleichbar der deutschen Stufe des Muschelkalks. Das Gestein ist in den ganzen Alpen verbreitet, mancherorts als Kalkstein (Calciumcarbonat), mancherorts als Dolomit mit einem zusätzlichen Anteil an Magnesium. Da bei der Dolomitisierung durch die Umkristallisation die Fossilspuren weitgehend gelöscht werden, sind im Wettersteindolomit die Fossilien noch schlechter, selbst im Dünnschliff kaum noch zu erkennen. Wettersteindolomit ist selten so bituminös und daher meist wesentlich reiner und hellfarbiger als der typische Hauptdolomit. Ansonsten sind keine grundsätzlichen Unterschiede zum gleichnamigen Kalk bekannt. Namensgebend war das Wettersteingebirge, weil der Wettersteinkalk hier besonders mächtige Berge bildet. Seinen Verbreitungsschwerpunkt besitzt er aber im Karwendel. In manchen Gegenden tritt ein engräumiger Wechsel von Kalk- und Dolomitfazies auf. Zu den Unterformen gehören , Schlerndolomit, , Steinalmkalk und Unterer Ramsaudolomit. , Steinalmkalk und Unterer Ramsaudolomit.
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Wettersteinkalk und Wettersteindolomit sin … Wettersteinkalk und Wettersteindolomit sind die häufigsten Namen für ein Karbonatgestein aus der Mittleren Trias, der ladinischen Zeitstufe, vergleichbar der deutschen Stufe des Muschelkalks. Das Gestein ist in den ganzen Alpen verbreitet, mancherorts als Kalkstein (Calciumcarbonat), mancherorts als Dolomit mit einem zusätzlichen Anteil an Magnesium. Da bei der Dolomitisierung durch die Umkristallisation die Fossilspuren weitgehend gelöscht werden, sind im Wettersteindolomit die Fossilien noch schlechter, selbst im Dünnschliff kaum noch zu erkennen. Wettersteindolomit ist selten so bituminös und daher meist wesentlich reiner und hellfarbiger als der typische Hauptdolomit. Ansonsten sind keine grundsätzlichen Unterschiede zum gleichnamigen Kalk bekannt.terschiede zum gleichnamigen Kalk bekannt.
, Wettersteinský vápenec (německy Wettersteinkalk, anglicky Wetterstein Limestone) je pevný, zpravidla (světle) šedý vápenec, středně až svrchnětriasového stáří (ladin-spodní karn). Představuje horninu typickou pro jižnější jednotky Alp, Karpat a Dinarid.
, The Wetterstein Formation is a regional ge … The Wetterstein Formation is a regional geologic formation of the Northern Limestone Alps and Western Carpathians extending from southern Bavaria, Germany in the west, through northern Austria to northern Hungary and western Slovakia in the east. The formation dates back to the Ladinian to Carnian stages of the Late Triassic. The formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians.stone Alps and in the Western Carpathians.
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, Wettersteinský vápenec
, Wetterstein Formation
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