The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data
Up to Jurassic times the Antarctic and African continents were part of the supercontinent Gondwana. Some 185 Ma the onset of rifting caused the dispersal of this vast continent into several minor plates. The timing and geometry of the initial break-up between Africa and Antarctica as well as the amo...
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ftawi:oai:epic.awi.de:38560 2024-09-09T19:04:26+00:00 The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data Mueller, Christian Olaf Schreckenberger, Bernd Heyde, Ingo Jokat, Wilfried 2015-12-15 application/pdf https://epic.awi.de/id/eprint/38560/ https://epic.awi.de/id/eprint/38560/1/Abstract_AGU_prep.pdf https://hdl.handle.net/10013/epic.45884 https://hdl.handle.net/10013/epic.45884.d001 unknown https://epic.awi.de/id/eprint/38560/1/Abstract_AGU_prep.pdf https://hdl.handle.net/10013/epic.45884.d001 Mueller, C. O. , Schreckenberger, B. , Heyde, I. and Jokat, W. orcid:0000-0002-7793-5854 (2015) The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data , AGU General Assembly, San Francisco, 14 December 2015 - 18 December 2015 . hdl:10013/epic.45884 EPIC3AGU General Assembly, San Francisco, 2015-12-14-2015-12-18 Conference notRev 2015 ftawi 2024-06-24T04:12:21Z Up to Jurassic times the Antarctic and African continents were part of the supercontinent Gondwana. Some 185 Ma the onset of rifting caused the dispersal of this vast continent into several minor plates. The timing and geometry of the initial break-up between Africa and Antarctica as well as the amount of volcanism connected to this Jurassic rifting are still controversial. In the southern part of the Mozambique Channel a prominent basement high, the Beira High, forms a distinct crustal anomaly along the Mozambican margin. It is still controversial if this area of shallow basement is a continental fragment or was formed during a period of enhanced magmatism and is of oceanic origin. Therefore, a wide-angle seismic profile with 37 OBS/H was acquired starting from the deep Mozambique Channel, across the Beira High and terminating on the shelf off the Zambezi River. The main objectives are to provide constraints on the crustal composition and origin of the Beira High as well as the amount of volcanism and the position of the continent-ocean transition below the Zambezi Delta. To obtain a P-wave velocity model of this area the data were forward modeled by means of the 2D-Raytracing method. Preliminary results indicate a clear thickening of the crust below the Beira High up to 20-24 km. Evidences for a high velocity body are found in the area below the Zambezi shelf with velocities of 7.2-7.4 km/s and up to 5 km thickness. Oceanic basement velocities at the very eastern part of the line start with values of 5.5 km/s, and increase to 6.9 km/s at lower crustal levels, that are typical for Jurassic oceanic crust. Across the Beira High the starting velocity and its gradient slightly change, presenting typical values for continental fragments. However, due to a sparse ray coverage of diving waves for the Beira High lower crust, these velocities still have to be proved. Thus, we will introduce the final results of a Finite Difference amplitude modeling, which will constrain the lowermost velocity gradients to allow a sound ... Conference Object Antarc* Antarctic Antarctica Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Antarctic The Antarctic |
institution |
Open Polar |
collection |
Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
Up to Jurassic times the Antarctic and African continents were part of the supercontinent Gondwana. Some 185 Ma the onset of rifting caused the dispersal of this vast continent into several minor plates. The timing and geometry of the initial break-up between Africa and Antarctica as well as the amount of volcanism connected to this Jurassic rifting are still controversial. In the southern part of the Mozambique Channel a prominent basement high, the Beira High, forms a distinct crustal anomaly along the Mozambican margin. It is still controversial if this area of shallow basement is a continental fragment or was formed during a period of enhanced magmatism and is of oceanic origin. Therefore, a wide-angle seismic profile with 37 OBS/H was acquired starting from the deep Mozambique Channel, across the Beira High and terminating on the shelf off the Zambezi River. The main objectives are to provide constraints on the crustal composition and origin of the Beira High as well as the amount of volcanism and the position of the continent-ocean transition below the Zambezi Delta. To obtain a P-wave velocity model of this area the data were forward modeled by means of the 2D-Raytracing method. Preliminary results indicate a clear thickening of the crust below the Beira High up to 20-24 km. Evidences for a high velocity body are found in the area below the Zambezi shelf with velocities of 7.2-7.4 km/s and up to 5 km thickness. Oceanic basement velocities at the very eastern part of the line start with values of 5.5 km/s, and increase to 6.9 km/s at lower crustal levels, that are typical for Jurassic oceanic crust. Across the Beira High the starting velocity and its gradient slightly change, presenting typical values for continental fragments. However, due to a sparse ray coverage of diving waves for the Beira High lower crust, these velocities still have to be proved. Thus, we will introduce the final results of a Finite Difference amplitude modeling, which will constrain the lowermost velocity gradients to allow a sound ... |
format |
Conference Object |
author |
Mueller, Christian Olaf Schreckenberger, Bernd Heyde, Ingo Jokat, Wilfried |
spellingShingle |
Mueller, Christian Olaf Schreckenberger, Bernd Heyde, Ingo Jokat, Wilfried The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data |
author_facet |
Mueller, Christian Olaf Schreckenberger, Bernd Heyde, Ingo Jokat, Wilfried |
author_sort |
Mueller, Christian Olaf |
title |
The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data |
title_short |
The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data |
title_full |
The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data |
title_fullStr |
The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data |
title_full_unstemmed |
The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data |
title_sort |
crustal structure of beira high, central mozambique – combined investigation of wide-angle seismic and potential field data |
publishDate |
2015 |
url |
https://epic.awi.de/id/eprint/38560/ https://epic.awi.de/id/eprint/38560/1/Abstract_AGU_prep.pdf https://hdl.handle.net/10013/epic.45884 https://hdl.handle.net/10013/epic.45884.d001 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Antarctica |
genre_facet |
Antarc* Antarctic Antarctica |
op_source |
EPIC3AGU General Assembly, San Francisco, 2015-12-14-2015-12-18 |
op_relation |
https://epic.awi.de/id/eprint/38560/1/Abstract_AGU_prep.pdf https://hdl.handle.net/10013/epic.45884.d001 Mueller, C. O. , Schreckenberger, B. , Heyde, I. and Jokat, W. orcid:0000-0002-7793-5854 (2015) The crustal structure of Beira High, Central Mozambique – Combined investigation of wide-angle seismic and potential field data , AGU General Assembly, San Francisco, 14 December 2015 - 18 December 2015 . hdl:10013/epic.45884 |
_version_ |
1809818449975705600 |