Matches in DBpedia 2016-04 for { ?s ?p "Santo Domingo Formation (Spanish: Formación Santo Domingo) is a mainly marine Miocene sedimentary formation located in south–central Chile. The formation was defined by R. Matínez-Pardo and Mario Pino in 1979 and named after the roadcut locality they studied about 19 km south-east of Valdivia. Sediments of the formation accumulated in Valdivia and Osorno–Llanquihue Basin.The formations overlies the basement of metamorphic and igneous rocks, that is Bahía Mansa Metamorphic Complex and Cretaceous granitoids respectively. In parts it further overlies the coal–bearing Pupunahue–Catamutún Formation. The sedimentary facies of Santo Domingo Formation are composed of sandstone, siltstone and mudstone plus smaller amounts of conglomerate. The formation underlies Pliocene and Quaternary sediments."@en }
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- Santo_Domingo_Formation abstract "Santo Domingo Formation (Spanish: Formación Santo Domingo) is a mainly marine Miocene sedimentary formation located in south–central Chile. The formation was defined by R. Matínez-Pardo and Mario Pino in 1979 and named after the roadcut locality they studied about 19 km south-east of Valdivia. Sediments of the formation accumulated in Valdivia and Osorno–Llanquihue Basin.The formations overlies the basement of metamorphic and igneous rocks, that is Bahía Mansa Metamorphic Complex and Cretaceous granitoids respectively. In parts it further overlies the coal–bearing Pupunahue–Catamutún Formation. The sedimentary facies of Santo Domingo Formation are composed of sandstone, siltstone and mudstone plus smaller amounts of conglomerate. The formation underlies Pliocene and Quaternary sediments.".
- Q21044399 abstract "Santo Domingo Formation (Spanish: Formación Santo Domingo) is a mainly marine Miocene sedimentary formation located in south–central Chile. The formation was defined by R. Matínez-Pardo and Mario Pino in 1979 and named after the roadcut locality they studied about 19 km south-east of Valdivia. Sediments of the formation accumulated in Valdivia and Osorno–Llanquihue Basin.The formations overlies the basement of metamorphic and igneous rocks, that is Bahía Mansa Metamorphic Complex and Cretaceous granitoids respectively. In parts it further overlies the coal–bearing Pupunahue–Catamutún Formation. The sedimentary facies of Santo Domingo Formation are composed of sandstone, siltstone and mudstone plus smaller amounts of conglomerate. The formation underlies Pliocene and Quaternary sediments.".