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Statements

Subject Item
dbr:Mazantic_Shale
rdf:type
dbo:MilitaryUnit
rdfs:label
Mazantic Shale Mazantic-Schiefer
rdfs:comment
Mazantic-Schiefer (engl.: Mazantic Shale;) ist ein Bernstein-führender Schiefer, der in der Periode des Neogen entstanden ist. Er gehört zur Formation des Chiapas Thrust-Fold Belt (Central & Eastern Thrust-fold Belt) in Mexiko und zeichnet sich durch eine große Anzahl von Insekten-Fossilien (Chiapas-Bernstein) aus. Der Mazantic-Schiefer wird von Balumtum-Sandstein überlagert. The Mazantic Shale is a geologic formation in Chiapas, Mexico. It was deposited during the Early Miocene (Aquitanian). The formation comprises dark gray shales that were deposited in a marine environment. It preserves fossils, such as the turtle Allaeochelys liliae. Amber has been recovered from it.
dbp:name
Mazantic Shale
dcterms:subject
dbc:Neogene_Mexico dbc:Shale_formations
dbo:wikiPageID
43328339
dbo:wikiPageRevisionID
1105502603
dbo:wikiPageWikiLink
dbr:Mexico dbr:List_of_fossiliferous_stratigraphic_units_in_Mexico dbr:Chiapas dbr:Shale dbr:Fossils dbr:Formation_(stratigraphy) dbc:Shale_formations dbr:Allaeochelys dbr:Amber dbc:Neogene_Mexico dbr:La_Quinta_Formation,_Mexico dbr:Turtle dbr:Formation_(geology) dbr:Miocene dbr:Balumtum_Sandstone dbr:Aquitanian_(stage)
owl:sameAs
wikidata:Q18358386 n9:miAD yago-res:Mazantic_Shale dbpedia-de:Mazantic-Schiefer freebase:m.01180dfb
dbp:underlies
dbr:Balumtum_Sandstone
dbp:wikiPageUsesTemplate
dbt:Short_description dbt:Reflist dbt:Mexico-geologic-formation-stub dbt:Infobox_rockunit dbt:Portal dbt:Fossilrange dbt:Neogene-stub
dbp:age
dbr:Miocene
dbp:country
dbr:Mexico
dbp:period
Miocene
dbp:thickness
310 m
dbp:type
dbr:Formation_(stratigraphy)
dbo:abstract
The Mazantic Shale is a geologic formation in Chiapas, Mexico. It was deposited during the Early Miocene (Aquitanian). The formation comprises dark gray shales that were deposited in a marine environment. It preserves fossils, such as the turtle Allaeochelys liliae. Amber has been recovered from it. Mazantic-Schiefer (engl.: Mazantic Shale;) ist ein Bernstein-führender Schiefer, der in der Periode des Neogen entstanden ist. Er gehört zur Formation des Chiapas Thrust-Fold Belt (Central & Eastern Thrust-fold Belt) in Mexiko und zeichnet sich durch eine große Anzahl von Insekten-Fossilien (Chiapas-Bernstein) aus. Der Schiefer kommt im Gebiet von Simojovel in Chiapas, Südwest-Mexiko vor. Er ist zum Beispiel in den Totalapa Amber bearing Beds zugänglich. Man geht davon aus, dass die Ablagerungen im Miozän, speziell in den Abschnitten des Burdigalium (21 – 16 Millionen Jahre), entstanden sind.Molluskenfunde und Gliederfüßer-Einschlüsse im Bernstein, sowie Lignite deuten darauf hin, dass es sich um kontinentale Ablagerungen handelt. Der Mazantic-Schiefer wird von Balumtum-Sandstein überlagert.
dbp:overlies
dbr:La_Quinta_Formation,_Mexico
dbp:prilithology
dbr:Shale
gold:hypernym
dbr:Formation
prov:wasDerivedFrom
wikipedia-en:Mazantic_Shale?oldid=1105502603&ns=0
dbo:wikiPageLength
2058
foaf:isPrimaryTopicOf
wikipedia-en:Mazantic_Shale