About: Apulia Carbonate Platform

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The Apulia Carbonate Platform in Apulia, Italy, was a major palaeogeographic element of the southern margin of the Mesozoic Tethys Ocean. It is one of the so-called peri-Adriatic platforms, which are comparable to the Bahama Banks in their carbonate facies, shape, size, and subsidence rate and, also, in the internal architecture.

Attributes	Values
rdf:type	military unit
rdfs:label	Apulia Carbonate Platform (en)
rdfs:comment	The Apulia Carbonate Platform in Apulia, Italy, was a major palaeogeographic element of the southern margin of the Mesozoic Tethys Ocean. It is one of the so-called peri-Adriatic platforms, which are comparable to the Bahama Banks in their carbonate facies, shape, size, and subsidence rate and, also, in the internal architecture. (en)
dct:subject	Geography of Apulia
Wikipage page ID	8988682 (xsd:integer)
Wikipage revision ID	1116943047 (xsd:integer)
Link from a Wikipage to another Wikipage	Cagnano Varano San Giovanni Rotondo Sannicandro di Bari Geography of Apulia Umbria Limestone Conoco Eocene Miocene Apennine Mountains Apricena Apulia Lutetian Manfredonia Callovian Burano Cenomanian Gargano Adriatic Albian Early Cretaceous Facies Breccia Carbonate platform AGIP Ionian Sea Italy Bahama Banks Tethys Ocean Jurassic Thrust fault Marche Mesozoic Terrigenous Upper Triassic Evaporite Palaeogeography Subsidence Stratigraphic Upper Jurassic Foresta Umbra
sameAs	Apulia Carbonate Platform Apulia Carbonate Platform Apulia Carbonate Platform
dbp:wikiPageUsesTemplate	dbt:Reflist
has abstract	The Apulia Carbonate Platform in Apulia, Italy, was a major palaeogeographic element of the southern margin of the Mesozoic Tethys Ocean. It is one of the so-called peri-Adriatic platforms, which are comparable to the Bahama Banks in their carbonate facies, shape, size, and subsidence rate and, also, in the internal architecture. The Apulia Platform, which is part of the stable and relatively undeformed foreland of the Apennine thrust belt, is bounded on both sides by basinal deposits; westward the margin is buried under the Apennine thrust sheets, to the east the adjacent paleogeographic domains are the vast Ionian Basin to the south and the Umbria-Marche Basin to the north. To the west, the Apulia Platform plunges downfaulted underneath the terrigenous sediments of the Apennine foredeep; to the southeast, the Jurassic–Early Cretaceous margin lies 20–30 km offshore from the present Apulia coastline. (en)
gold:hypernym	Element
prov:wasDerivedFrom	wikipedia-en:Apulia_Carbonate_Platform?oldid=1116943047&ns=0
page length (characters) of wiki page	8112 (xsd:nonNegativeInteger)
foaf:isPrimaryTopicOf	wikipedia-en:Apulia_Carbonate_Platform
is Link from a Wikipage to another Wikipage of	Barletta Resolution Guyot Geology of Croatia 2002 Molise earthquakes Adriatic Sea Southern Italy Apulia Platform Promontorio del Gargano Gargano Peninsula Gargano Promontory Gargano geology
is Wikipage redirect of	Apulia Platform Promontorio del Gargano Gargano Peninsula Gargano Promontory Gargano geology
is foaf:primaryTopic of	wikipedia-en:Apulia_Carbonate_Platform

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