Reconstruction of the East Africa and Antarctica continental margins

The Early Jurassic separation of Antarctica from Africa plays an important role in our understanding of the dispersal of Gondwana and Pangea. Previous reconstruction models contain overlaps and gaps in the restored margins that reflect difficulties in accurately delineating the continent‐ocean‐bound...

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Veröffentlicht in:	Journal of geophysical research. Solid earth Jg. 121; H. 6; S. 4156 - 4179
Hauptverfasser:	Nguyen, Luan C., Hall, Stuart A., Bird, Dale E., Ball, Philip J.
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	Washington Blackwell Publishing Ltd 01.06.2016
Schlagworte:	Antarctica Coastal plains Coasts Cob Continental crust Continental margins Correlation Crustal thickness Crusts Direction Dispersal Dispersion Distribution Drift Evolution Fracture mechanics Fracture zones Geophysics Gravitation Gravity Gravity data Identification Jurassic Magma Marine Methods Mozambique Ocean floor Oceanic crust Pangea plate tectonics Reconstruction restoration rifted margins Rifting Satellites Seafloor spreading Seismology Separation Spreading Three dimensional models volcanics East Africa Antarctica Pangea PS, Antarctica ISW, Mozambique Africa
ISSN:	2169-9313, 2169-9356
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Abstract	The Early Jurassic separation of Antarctica from Africa plays an important role in our understanding of the dispersal of Gondwana and Pangea. Previous reconstruction models contain overlaps and gaps in the restored margins that reflect difficulties in accurately delineating the continent‐ocean‐boundary (COB) and determining the amount and distribution of extended continental crust. This study focuses on the evolution of the African margin adjacent to the Mozambique Basin and the conjugate Antarctic margin near the Riiser‐Larsen Sea. Satellite‐derived gravity data have been used to trace the orientations and landward limits of fracture zones. A 3‐D gravity inversion has produced a crustal thickness model that reliably quantifies the extent and amount of stretched crust. Crustal thicknesses together with fracture zone terminations reveal COBs that are significantly closer to the African and Antarctic coasts than previously recognized. Correlation of fracture zone azimuths and identified COBs suggests Antarctica began drifting away from Africa at approximately 171 Ma in a roughly SSE direction. An areal‐balancing method has been used to restore the crust to a uniform prerift thickness so as to perform a nonrigid reconstruction for both nonvolcanic and volcanic margins. Both margins reveal a trend of increasing extension from east to west. Our results suggest Africa underwent extension of 60–120 km, while Antarctic crust was stretched by 105–180 km. Various models tested to determine the direction of extension during rifting suggest that Antarctica moved away from Africa in a WNW‐ESE direction during the period between 184 and 171 Ma prior to the onset of seafloor spreading. Key Points Early Jurassic rifting between Africa and Antarctica took place in a WNW‐ESE direction Eastern part of the Mozambique Coastal Plain is underlain by oceanic crust
AbstractList	The Early Jurassic separation of Antarctica from Africa plays an important role in our understanding of the dispersal of Gondwana and Pangea. Previous reconstruction models contain overlaps and gaps in the restored margins that reflect difficulties in accurately delineating the continent-ocean-boundary (COB) and determining the amount and distribution of extended continental crust. This study focuses on the evolution of the African margin adjacent to the Mozambique Basin and the conjugate Antarctic margin near the Riiser-Larsen Sea. Satellite-derived gravity data have been used to trace the orientations and landward limits of fracture zones. A 3-D gravity inversion has produced a crustal thickness model that reliably quantifies the extent and amount of stretched crust. Crustal thicknesses together with fracture zone terminations reveal COBs that are significantly closer to the African and Antarctic coasts than previously recognized. Correlation of fracture zone azimuths and identified COBs suggests Antarctica began drifting away from Africa at approximately 171Ma in a roughly SSE direction. An areal-balancing method has been used to restore the crust to a uniform prerift thickness so as to perform a nonrigid reconstruction for both nonvolcanic and volcanic margins. Both margins reveal a trend of increasing extension from east to west. Our results suggest Africa underwent extension of 60-120km, while Antarctic crust was stretched by 105-180km. Various models tested to determine the direction of extension during rifting suggest that Antarctica moved away from Africa in a WNW-ESE direction during the period between 184 and 171Ma prior to the onset of seafloor spreading. Key Points Early Jurassic rifting between Africa and Antarctica took place in a WNW-ESE direction Eastern part of the Mozambique Coastal Plain is underlain by oceanic crust The Early Jurassic separation of Antarctica from Africa plays an important role in our understanding of the dispersal of Gondwana and Pangea. Previous reconstruction models contain overlaps and gaps in the restored margins that reflect difficulties in accurately delineating the continent‐ocean‐boundary (COB) and determining the amount and distribution of extended continental crust. This study focuses on the evolution of the African margin adjacent to the Mozambique Basin and the conjugate Antarctic margin near the Riiser‐Larsen Sea. Satellite‐derived gravity data have been used to trace the orientations and landward limits of fracture zones. A 3‐D gravity inversion has produced a crustal thickness model that reliably quantifies the extent and amount of stretched crust. Crustal thicknesses together with fracture zone terminations reveal COBs that are significantly closer to the African and Antarctic coasts than previously recognized. Correlation of fracture zone azimuths and identified COBs suggests Antarctica began drifting away from Africa at approximately 171 Ma in a roughly SSE direction. An areal‐balancing method has been used to restore the crust to a uniform prerift thickness so as to perform a nonrigid reconstruction for both nonvolcanic and volcanic margins. Both margins reveal a trend of increasing extension from east to west. Our results suggest Africa underwent extension of 60–120 km, while Antarctic crust was stretched by 105–180 km. Various models tested to determine the direction of extension during rifting suggest that Antarctica moved away from Africa in a WNW‐ESE direction during the period between 184 and 171 Ma prior to the onset of seafloor spreading. Early Jurassic rifting between Africa and Antarctica took place in a WNW‐ESE direction Eastern part of the Mozambique Coastal Plain is underlain by oceanic crust The Early Jurassic separation of Antarctica from Africa plays an important role in our understanding of the dispersal of Gondwana and Pangea. Previous reconstruction models contain overlaps and gaps in the restored margins that reflect difficulties in accurately delineating the continent‐ocean‐boundary (COB) and determining the amount and distribution of extended continental crust. This study focuses on the evolution of the African margin adjacent to the Mozambique Basin and the conjugate Antarctic margin near the Riiser‐Larsen Sea. Satellite‐derived gravity data have been used to trace the orientations and landward limits of fracture zones. A 3‐D gravity inversion has produced a crustal thickness model that reliably quantifies the extent and amount of stretched crust. Crustal thicknesses together with fracture zone terminations reveal COBs that are significantly closer to the African and Antarctic coasts than previously recognized. Correlation of fracture zone azimuths and identified COBs suggests Antarctica began drifting away from Africa at approximately 171 Ma in a roughly SSE direction. An areal‐balancing method has been used to restore the crust to a uniform prerift thickness so as to perform a nonrigid reconstruction for both nonvolcanic and volcanic margins. Both margins reveal a trend of increasing extension from east to west. Our results suggest Africa underwent extension of 60–120 km, while Antarctic crust was stretched by 105–180 km. Various models tested to determine the direction of extension during rifting suggest that Antarctica moved away from Africa in a WNW‐ESE direction during the period between 184 and 171 Ma prior to the onset of seafloor spreading. Key Points Early Jurassic rifting between Africa and Antarctica took place in a WNW‐ESE direction Eastern part of the Mozambique Coastal Plain is underlain by oceanic crust
Author	Nguyen, Luan C. Bird, Dale E. Hall, Stuart A. Ball, Philip J.
Author_xml	– sequence: 1 givenname: Luan C. surname: Nguyen fullname: Nguyen, Luan C. organization: University of Houston – sequence: 2 givenname: Stuart A. surname: Hall fullname: Hall, Stuart A. organization: University of Houston – sequence: 3 givenname: Dale E. surname: Bird fullname: Bird, Dale E. organization: Bird Geophysical – sequence: 4 givenname: Philip J. surname: Ball fullname: Ball, Philip J. organization: ConocoPhillips Company
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Snippet	The Early Jurassic separation of Antarctica from Africa plays an important role in our understanding of the dispersal of Gondwana and Pangea. Previous...
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SubjectTerms	Antarctica Coastal plains Coasts Cob Continental crust Continental margins Correlation Crustal thickness Crusts Direction Dispersal Dispersion Distribution Drift Evolution Fracture mechanics Fracture zones Geophysics Gravitation Gravity Gravity data Identification Jurassic Magma Marine Methods Mozambique Ocean floor Oceanic crust Pangea plate tectonics Reconstruction restoration rifted margins Rifting Satellites Seafloor spreading Seismology Separation Spreading Three dimensional models volcanics
Title	Reconstruction of the East Africa and Antarctica continental margins
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