Aimal Kasi, Akhtar Kasi:Sedimentology of the Neogene Strata in Pishin Belt, Western Pakistan
- Livres de poche 2001, ISBN: 9786139842346
[ED: Taschenbuch], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren - The Neogene succession of the Pishin Belt occupies the area along the northwestern margin o… Plus…
[ED: Taschenbuch], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren - The Neogene succession of the Pishin Belt occupies the area along the northwestern margin of Pakistan. Western boundary of the belt is transpressional with the Afghan Block due to the Chaman Fault, while its eastern and southeastern boundary is dominantly compressional. The Zhob Valley Thrust separates the Pishin Belt from the Sulaiman Fold-Thrust Belt of the Indian Plate. The belt is divisible into six tectono-stratigraphic zones, having its distinct lithostratigraphy and bounded by major thrusts and/or unconformities. The Muslim Bagh-Zhob Ophiolite marks the base, and Zone-I of the belt. The Eocene Nisai Formation and the Oligocene-Early Miocene Khojak Formation, makes our Zone-II, which overlies the Muslim Bagh-Zhob Ophiolite with a non-conformable contact. The Early-Middle Miocene Dasht Murgha group overlies the Nisai Formation with angular unconformity and constitutes Zone-III. The Late Miocene-Pliocene Malthanai formation makes Zone-IV and its lower and upper contacts with the Nisai Formation are thrusted. The Pleistocene Bostan Formation, having a thrust contact with the Malthanai formation, DE, [SC: 3.00], leichte Gebrauchsspuren, gewerbliches Angebot, 220x150x14 mm, 228, [GW: 358g], Banküberweisung, PayPal, Internationaler Versand<
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Aimal Kasi, Akhtar Kasi:Sedimentology of the Neogene Strata in Pishin Belt, Western Pakistan
- Livres de poche 2018, ISBN: 6139842344
[EAN: 9786139842346], [SC: 9.82], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren -The Neogene succession of the Pishin Belt occupies the area along the northwe… Plus…
[EAN: 9786139842346], [SC: 9.82], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren -The Neogene succession of the Pishin Belt occupies the area along the northwestern margin of Pakistan. Western boundary of the belt is transpressional with the Afghan Block due to the Chaman Fault, while its eastern and southeastern boundary is dominantly compressional. The Zhob Valley Thrust separates the Pishin Belt from the Sulaiman Fold-Thrust Belt of the Indian Plate. The belt is divisible into six tectono-stratigraphic zones, having its distinct lithostratigraphy and bounded by major thrusts and/or unconformities. The Muslim Bagh-Zhob Ophiolite marks the base, and Zone-I of the belt. The Eocene Nisai Formation and the Oligocene-Early Miocene Khojak Formation, makes our Zone-II, which overlies the Muslim Bagh-Zhob Ophiolite with a non-conformable contact. The Early-Middle Miocene Dasht Murgha group overlies the Nisai Formation with angular unconformity and constitutes Zone-III. The Late Miocene-Pliocene Malthanai formation makes Zone-IV and its lower and upper contacts with the Nisai Formation are thrusted. The Pleistocene Bostan Formation, having a thrust contact with the Malthanai formation 228 pp. Englisch, Books<
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(*) Livre non disponible signifie que le livre est actuellement pas disponible à l'une des plates-formes associées nous recherche.
Aimal Kasi, Akhtar Kasi:Sedimentology of the Neogene Strata in Pishin Belt, Western Pakistan
- Livres de poche 2018, ISBN: 6139842344
[EAN: 9786139842346], [SC: 0.0], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren -The Neogene succession of the Pishin Belt occupies the area along the northwes… Plus…
[EAN: 9786139842346], [SC: 0.0], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren -The Neogene succession of the Pishin Belt occupies the area along the northwestern margin of Pakistan. Western boundary of the belt is transpressional with the Afghan Block due to the Chaman Fault, while its eastern and southeastern boundary is dominantly compressional. The Zhob Valley Thrust separates the Pishin Belt from the Sulaiman Fold-Thrust Belt of the Indian Plate. The belt is divisible into six tectono-stratigraphic zones, having its distinct lithostratigraphy and bounded by major thrusts and/or unconformities. The Muslim Bagh-Zhob Ophiolite marks the base, and Zone-I of the belt. The Eocene Nisai Formation and the Oligocene-Early Miocene Khojak Formation, makes our Zone-II, which overlies the Muslim Bagh-Zhob Ophiolite with a non-conformable contact. The Early-Middle Miocene Dasht Murgha group overlies the Nisai Formation with angular unconformity and constitutes Zone-III. The Late Miocene-Pliocene Malthanai formation makes Zone-IV and its lower and upper contacts with the Nisai Formation are thrusted. The Pleistocene Bostan Formation, having a thrust contact with the Malthanai formation 228 pp. Englisch, Books<
| | ZVAB.comRheinberg-Buch Andreas Meier eK, Bergisch Gladbach, Germany [53870650] [Rating: 5 (von 5)] Frais d'envoiVersandkostenfrei. (EUR 0.00) Details... |
(*) Livre non disponible signifie que le livre est actuellement pas disponible à l'une des plates-formes associées nous recherche.
Aimal Kasi, Akhtar Kasi:Sedimentology of the Neogene Strata in Pishin Belt, Western Pakistan
- Livres de poche 2018, ISBN: 6139842344
[EAN: 9786139842346], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren -The Neogene succession of the Pishin Belt occupies the area along the northwestern margin… Plus…
[EAN: 9786139842346], [PU: LAP LAMBERT Academic Publishing], Gebraucht - Gut Leichte Lagerspuren -The Neogene succession of the Pishin Belt occupies the area along the northwestern margin of Pakistan. Western boundary of the belt is transpressional with the Afghan Block due to the Chaman Fault, while its eastern and southeastern boundary is dominantly compressional. The Zhob Valley Thrust separates the Pishin Belt from the Sulaiman Fold-Thrust Belt of the Indian Plate. The belt is divisible into six tectono-stratigraphic zones, having its distinct lithostratigraphy and bounded by major thrusts and/or unconformities. The Muslim Bagh-Zhob Ophiolite marks the base, and Zone-I of the belt. The Eocene Nisai Formation and the Oligocene-Early Miocene Khojak Formation, makes our Zone-II, which overlies the Muslim Bagh-Zhob Ophiolite with a non-conformable contact. The Early-Middle Miocene Dasht Murgha group overlies the Nisai Formation with angular unconformity and constitutes Zone-III. The Late Miocene-Pliocene Malthanai formation makes Zone-IV and its lower and upper contacts with the Nisai Formation are thrusted. The Pleistocene Bostan Formation, having a thrust contact with the Malthanai formation 228 pp. Englisch, Books<
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Kasi, Aimal; Kasi, Akhtar:Sedimentology of the Neogene Strata in Pishin Belt, Western Pakistan
- nouveau livre 2018, ISBN: 6139842344
Kartoniert / Broschiert, mit Schutzumschlag 11, [PU:LAP LAMBERT Academic Publishing]
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