Discovery of Late Triassic fossils in the Chonos Metamorphic Complex, Southern Chile

Zonq Jie Fang, Arthur Boucot, Vladimir Covacevich, Francisco Hervé

Resultado de la investigación: Article

32 Citas (Scopus)

Resumen

The late Triassic bivalve Monotis (Pacimonolis) aft. subcircularis Gabb indicative of a Norian (probably early late Norian) age has been collected from the southeastern end of Patranca Island (45°25'S-74°09'W) in the Chonos Archipelago, Southern Chile. Another fossil bivalve, Limidae gen. et sp. indet. has been collected from a small unnamed island (45°25'S-74° 10'W) 4 km to the north, and indicates a maximum Early Carboniferous, probably Mesozoic age. The fossil bearing unit is the Potranca Formation (or Potranca Unit) which forms part of the Chonos Metamorphic Complex, interpreted as a subduction complex developed on the southwestern margin of Gondwanaland. As these rocks have been previously considered to be of Paleozoic age (Late Silurian-Early Devonian), the geologic history of this part of the continental margin must be reinterpreted. These fossils provide clear evidence that marine depositional processes persisted within the Chonos Metamorphic Complex during Late Triassic time.

Idioma originalEnglish
Páginas (desde-hasta)165-173
Número de páginas9
PublicaciónRevista Geologica de Chile
Volumen25
N.º2
EstadoPublished - 1998

Huella dactilar

Bearings (structural)
Norian
Triassic
Rocks
fossil
bivalve
Silurian
archipelago
continental margin
subduction
Paleozoic
history
rock

ASJC Scopus subject areas

  • Geology

Citar esto

Fang, Zonq Jie ; Boucot, Arthur ; Covacevich, Vladimir ; Hervé, Francisco. / Discovery of Late Triassic fossils in the Chonos Metamorphic Complex, Southern Chile. En: Revista Geologica de Chile. 1998 ; Vol. 25, N.º 2. pp. 165-173.
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abstract = "The late Triassic bivalve Monotis (Pacimonolis) aft. subcircularis Gabb indicative of a Norian (probably early late Norian) age has been collected from the southeastern end of Patranca Island (45°25'S-74°09'W) in the Chonos Archipelago, Southern Chile. Another fossil bivalve, Limidae gen. et sp. indet. has been collected from a small unnamed island (45°25'S-74° 10'W) 4 km to the north, and indicates a maximum Early Carboniferous, probably Mesozoic age. The fossil bearing unit is the Potranca Formation (or Potranca Unit) which forms part of the Chonos Metamorphic Complex, interpreted as a subduction complex developed on the southwestern margin of Gondwanaland. As these rocks have been previously considered to be of Paleozoic age (Late Silurian-Early Devonian), the geologic history of this part of the continental margin must be reinterpreted. These fossils provide clear evidence that marine depositional processes persisted within the Chonos Metamorphic Complex during Late Triassic time.",
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Discovery of Late Triassic fossils in the Chonos Metamorphic Complex, Southern Chile. / Fang, Zonq Jie; Boucot, Arthur; Covacevich, Vladimir; Hervé, Francisco.

En: Revista Geologica de Chile, Vol. 25, N.º 2, 1998, p. 165-173.

Resultado de la investigación: Article

TY - JOUR

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AU - Boucot, Arthur

AU - Covacevich, Vladimir

AU - Hervé, Francisco

PY - 1998

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