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Title of Thesis
CRUSTAL MODELING OF BANNU-KOHAT AREA WITH THE HELP OF INTEGRATED GEOPHYSICAL DATA |
Author(s)
SHAMS-UD-DIN |
Institute/University/Department Details
Department of Earth Sciences/ Quaid-i-Azam University, Islamabad |
Session
2007 |
Subject
Earth Sciences |
Number of Pages
59 |
Keywords (Extracted from title, table of contents and abstract of thesis)
crustal modeling, kohat plateau, bannu basin, tm image data, gravity data, isostatic model |
Abstract Gross crustal structures of Kohat plateau and Bannu basin area have been interpreted incorporating gravity, seismicity and landsat TM image data. The continued northward movement of the Indian plate against the Euorasian plate has produced litho-structural complexities in the area. The analysis shows that most of the area is dominantly a thin skinned type of fold and thrust belt. Basement faulting is confined to a small western part of the Kohat plateau and Mianwali reentrant. The major thrust faults are due to the presence of basal decollement between the sediments and the basement. Some blind/ hidden faults or micro shear zones exist. Gravity model BB' show two such faults named Adughar and Akhun Kot faults, while model CC' indicate Karak fault to extend further south east. There are indications from the Bouguer, Residual gravity and landsat TM image data that Kalabagh fault may be extending further north. The 2-D gravity models suggest the thickening of the crust 38 km in the south to more than 45 km in the north and northwest. A comparison of isostatic moho with the gravimetric moho shows that areas lying southeast including the Salt range are over-compensated due to the thinning of the crust, whereas the Kohat- Potwar plateau areas, Bannu basin and Mianwali reentrant are under-compensated.
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Chapter |
Title of the Chapters |
Page |
Size (KB) |
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| 1 |
0 |
Contents |
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 75.14 KB |
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| 2 |
1 |
Introduction |
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 89.21 KB |
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1.1 |
Introduction |
1 |
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1.2 |
Purpose And Scope Of Work |
1 |
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1.3 |
Previous Work |
3 |
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| 3 |
2 |
General Geology And Stratigrapgy |
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 482.32 KB |
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2.1 |
Regional Geology |
5 |
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2.2 |
Regional Tectonics |
8 |
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2.3 |
Stratigraphy |
12 |
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| 4 |
3 |
Geomorphologic Landsat TM Image Analysis And Neotectonic Studies |
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 177.5 KB |
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3.1 |
Introduction |
16 |
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3.2 |
Critical Seismotectonic Features Of The Area (Fig. 3.2) |
19 |
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| 5 |
4 |
Description Of Gravity Maps |
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 417.14 KB |
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4.1 |
Gravity Data |
23 |
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4.2 |
Bouguer Anomaly Map |
23 |
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4.3 |
Regional Gravity Anomaly Map |
25 |
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4.4 |
Upward-Continuation Filter |
27 |
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4.5 |
Residual Gravity Anomaly Map |
32 |
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| 6 |
5 |
Interpretation Of 2-D Gravity Models And Some Isostatic |
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 925.86 KB |
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5.1 |
Introduction |
34 |
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5.2 |
2-D Gravity Model Along Profile A-A’ |
35 |
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5.3 |
2-D Gravity Model Along Profile B-B’ |
35 |
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5.4 |
2-D Gravity Model Along Profile C-C’ |
36 |
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5.5 |
Isostatic Model |
40 |
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| 7 |
6 |
Discussion Of Results |
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 39.51 KB |
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6.1 |
Discussion |
48 |
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6.2 |
Conclusions |
49 |
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| 8 |
7 |
References |
51 |
 207.13 KB |
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7.1 |
Appendix |
59 |
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