Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)

The Magellan Block, located on the modern Atlantic continental platform opposite the Strait of Magellan (Chile), consists of two parallel, northwest trending horsts partly separated by a central graben. Petroleum has been recovered from the Springhill Formation, deposited on this isolated platform d...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Sánchez,Jesús A., Le Roux,Jacobus P.
Lenguaje:English
Publicado: Servicio Nacional de Geología y Minería (SERNAGEOMIN) 2003
Materias:
Acceso en línea:http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082003000200001
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:scielo:S0716-02082003000200001
record_format dspace
spelling oai:scielo:S0716-020820030002000012004-04-22Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)Sánchez,Jesús A.Le Roux,Jacobus P. Supratidal Intertidal Barrier beach Shoreface Parasequence The Magellan Block, located on the modern Atlantic continental platform opposite the Strait of Magellan (Chile), consists of two parallel, northwest trending horsts partly separated by a central graben. Petroleum has been recovered from the Springhill Formation, deposited on this isolated platform during the Valanginian-Barremanian, since 1994. This formation represents an overall transgressive succession with three subcycles of transgression and regression (parasequences) separated by marine flooding surfaces. The two basal parasequences are related either to minor sea level fluctuations or to fault activity, whereas the uppermost cycle reflects a major transgression affecting the whole Magellan Basin. Depositional facies associations include supratidal, intertidal, barrier beach and shoreface environments, generally showing a clear correlation with the paleotopography of the horst blocks. While barrier beaches formed along the topographically higher areas, inter- and supratidal flats and shoreface sediments were deposited on their land- and seaward sides, respectively. Tidal flats also bordered the shallow embayment formed by the central graben. Continued transgression subsequently drowned the island to form a wide, open platform on which the Estratos con Fravella Formation was depositedinfo:eu-repo/semantics/openAccessServicio Nacional de Geología y Minería (SERNAGEOMIN)Revista geológica de Chile v.30 n.2 20032003-12-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082003000200001en10.4067/S0716-02082003000200001
institution Scielo Chile
collection Scielo Chile
language English
topic Supratidal
Intertidal
Barrier beach
Shoreface
Parasequence
spellingShingle Supratidal
Intertidal
Barrier beach
Shoreface
Parasequence
Sánchez,Jesús A.
Le Roux,Jacobus P.
Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)
description The Magellan Block, located on the modern Atlantic continental platform opposite the Strait of Magellan (Chile), consists of two parallel, northwest trending horsts partly separated by a central graben. Petroleum has been recovered from the Springhill Formation, deposited on this isolated platform during the Valanginian-Barremanian, since 1994. This formation represents an overall transgressive succession with three subcycles of transgression and regression (parasequences) separated by marine flooding surfaces. The two basal parasequences are related either to minor sea level fluctuations or to fault activity, whereas the uppermost cycle reflects a major transgression affecting the whole Magellan Basin. Depositional facies associations include supratidal, intertidal, barrier beach and shoreface environments, generally showing a clear correlation with the paleotopography of the horst blocks. While barrier beaches formed along the topographically higher areas, inter- and supratidal flats and shoreface sediments were deposited on their land- and seaward sides, respectively. Tidal flats also bordered the shallow embayment formed by the central graben. Continued transgression subsequently drowned the island to form a wide, open platform on which the Estratos con Fravella Formation was deposited
author Sánchez,Jesús A.
Le Roux,Jacobus P.
author_facet Sánchez,Jesús A.
Le Roux,Jacobus P.
author_sort Sánchez,Jesús A.
title Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)
title_short Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)
title_full Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)
title_fullStr Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)
title_full_unstemmed Mesozoic sedimentation on an isolated platform at the eastern entrance to the Strait of Magellan, Tierra del Fuego (Chile)
title_sort mesozoic sedimentation on an isolated platform at the eastern entrance to the strait of magellan, tierra del fuego (chile)
publisher Servicio Nacional de Geología y Minería (SERNAGEOMIN)
publishDate 2003
url http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082003000200001
work_keys_str_mv AT sanchezjesusa mesozoicsedimentationonanisolatedplatformattheeasternentrancetothestraitofmagellantierradelfuegochile
AT lerouxjacobusp mesozoicsedimentationonanisolatedplatformattheeasternentrancetothestraitofmagellantierradelfuegochile
_version_ 1718439418153402368