Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin
Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Farid, Asam [verfasserIn] Khalid, Perveiz [verfasserIn] Ali, Muhammad Y. [verfasserIn] Iqbal, Muhammad Asim [verfasserIn] Jadoon, Khan Zaib [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2017 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Geologische Rundschau - Berlin : Springer, 1910, 107(2017), 5 vom: 22. Nov., Seite 1557-1578 |
|---|---|
| Übergeordnetes Werk: |
volume:107 ; year:2017 ; number:5 ; day:22 ; month:11 ; pages:1557-1578 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00531-017-1558-6 |
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SPR006730035 |
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| 520 | |a Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. | ||
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10.1007/s00531-017-1558-6 doi (DE-627)SPR006730035 (SPR)s00531-017-1558-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Farid, Asam verfasserin aut Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. Flexure (dpeaa)DE-He213 Bulge (dpeaa)DE-He213 Seismic stratigraphy (dpeaa)DE-He213 Unconformities (dpeaa)DE-He213 Himalayas (dpeaa)DE-He213 Khalid, Perveiz verfasserin aut Ali, Muhammad Y. verfasserin aut Iqbal, Muhammad Asim verfasserin aut Jadoon, Khan Zaib verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 107(2017), 5 vom: 22. Nov., Seite 1557-1578 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:107 year:2017 number:5 day:22 month:11 pages:1557-1578 https://dx.doi.org/10.1007/s00531-017-1558-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 107 2017 5 22 11 1557-1578 |
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10.1007/s00531-017-1558-6 doi (DE-627)SPR006730035 (SPR)s00531-017-1558-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Farid, Asam verfasserin aut Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. Flexure (dpeaa)DE-He213 Bulge (dpeaa)DE-He213 Seismic stratigraphy (dpeaa)DE-He213 Unconformities (dpeaa)DE-He213 Himalayas (dpeaa)DE-He213 Khalid, Perveiz verfasserin aut Ali, Muhammad Y. verfasserin aut Iqbal, Muhammad Asim verfasserin aut Jadoon, Khan Zaib verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 107(2017), 5 vom: 22. Nov., Seite 1557-1578 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:107 year:2017 number:5 day:22 month:11 pages:1557-1578 https://dx.doi.org/10.1007/s00531-017-1558-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 107 2017 5 22 11 1557-1578 |
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10.1007/s00531-017-1558-6 doi (DE-627)SPR006730035 (SPR)s00531-017-1558-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Farid, Asam verfasserin aut Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. Flexure (dpeaa)DE-He213 Bulge (dpeaa)DE-He213 Seismic stratigraphy (dpeaa)DE-He213 Unconformities (dpeaa)DE-He213 Himalayas (dpeaa)DE-He213 Khalid, Perveiz verfasserin aut Ali, Muhammad Y. verfasserin aut Iqbal, Muhammad Asim verfasserin aut Jadoon, Khan Zaib verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 107(2017), 5 vom: 22. Nov., Seite 1557-1578 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:107 year:2017 number:5 day:22 month:11 pages:1557-1578 https://dx.doi.org/10.1007/s00531-017-1558-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 107 2017 5 22 11 1557-1578 |
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10.1007/s00531-017-1558-6 doi (DE-627)SPR006730035 (SPR)s00531-017-1558-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Farid, Asam verfasserin aut Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. Flexure (dpeaa)DE-He213 Bulge (dpeaa)DE-He213 Seismic stratigraphy (dpeaa)DE-He213 Unconformities (dpeaa)DE-He213 Himalayas (dpeaa)DE-He213 Khalid, Perveiz verfasserin aut Ali, Muhammad Y. verfasserin aut Iqbal, Muhammad Asim verfasserin aut Jadoon, Khan Zaib verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 107(2017), 5 vom: 22. Nov., Seite 1557-1578 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:107 year:2017 number:5 day:22 month:11 pages:1557-1578 https://dx.doi.org/10.1007/s00531-017-1558-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 107 2017 5 22 11 1557-1578 |
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10.1007/s00531-017-1558-6 doi (DE-627)SPR006730035 (SPR)s00531-017-1558-6-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Farid, Asam verfasserin aut Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin 2017 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. Flexure (dpeaa)DE-He213 Bulge (dpeaa)DE-He213 Seismic stratigraphy (dpeaa)DE-He213 Unconformities (dpeaa)DE-He213 Himalayas (dpeaa)DE-He213 Khalid, Perveiz verfasserin aut Ali, Muhammad Y. verfasserin aut Iqbal, Muhammad Asim verfasserin aut Jadoon, Khan Zaib verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 107(2017), 5 vom: 22. Nov., Seite 1557-1578 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:107 year:2017 number:5 day:22 month:11 pages:1557-1578 https://dx.doi.org/10.1007/s00531-017-1558-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 107 2017 5 22 11 1557-1578 |
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Farid, Asam |
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550 ASE 38.10 bkl Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin Flexure (dpeaa)DE-He213 Bulge (dpeaa)DE-He213 Seismic stratigraphy (dpeaa)DE-He213 Unconformities (dpeaa)DE-He213 Himalayas (dpeaa)DE-He213 |
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Seismic stratigraphy of the Mianwali and Bannu depressions, north-western Indus foreland basin |
| abstract |
Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. |
| abstractGer |
Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. |
| abstract_unstemmed |
Abstract Regional seismic reflection profiles, deep exploratory wells, and outcrop data have been used to study the structure and stratigraphic architecture of the Mianwali and Bannu depressions, north-western Indus foreland basin. Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. The tectonic activity reached to its maximum during Oligocene with the formation of a prominent unconformity, which caused extensive erosion that increases towards the flexural bulge. |
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Synthetic seismograms have been used to identify and tie the seismic horizons to the well data. Nine mappable seismic sequences are identified within the passive and active margin sediments. In general, the Mianwali and Bannu depressions deepens towards north due to the flexure generated by the loading and southward shifting of the thrust sheets of the North-western Himalayan Fold and Thrust Belt. The seismic profiles show a classic wedge shaped foreland basin with a prominent angular unconformity which clearly differentiates the active and passive margin sediments. The onlap patterns in the Late Cretaceous sediments suggest the initial onset of foreland basin formation when the Indian Plate collided with Eurasian Plate. As the collision progressed, the lithospheric flexure caused an uplift along the flexural bulge which resulted in onlaps within the Paleocene and Eocene sequences. 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