Paleogene carbonate ramp development in the Kohat Basin of northwestern Pakistan

References

• Adey, W. H., & Macintyre, I. G. (1973). Crustose coralline algae: A re-evaluation in the geological sciences. Geological Society of America Bulletin, 84(3), 883–904. https://doi.org/10.1130/0016-7606(1973)84<883:CCAARI>2.0.CO;2
   Web of Science ®Google Scholar
• Afzal, J., Khan, A. M., & Shafique, N. A. (1997). Biostratigraphy of Kirthar Formation (Middle to Late Eocene), Sulaiman Basin, Pakistan. Pakistan Journal of Hydrocarbon Research, 9, 15–33.
   Google Scholar
• Ahmad, S., Jalal, W., Ali, F., Hanif, M., Ullah, Z., Khan, S., Ali, A., Jan, I. U., & Rehman, K. (2015). Using larger benthic foraminifera for the paleogeographic reconstruction of Neo-Tethys during Paleogene. Arabian Journal of Geosciences, 8(7), 5095–5110. https://doi.org/10.1007/s12517-014-1549-x
   Web of Science ®Google Scholar
• Ahmad, S., Kroon, D., Rigby, S., & Khan, S. (2016). Paleogene Nummulitid biostratigraphyof the Kohat and Potwar basins in north-western Pakistan with implications for the timing of the closure of eastern Tethys and uplift of the western Himalayas. Stratigraphy, 13(4), 277–301.
   Web of Science ®Google Scholar
• Aigner, T. (1983). Facies and origin of nummulitic buildups: An example from the Giza Pyramids Plateau (Middle Eocene, Egypt). Neues Jahrbuch fur Geologie und Paläontologie – Abhandlungen, 166, 347–368.
   Google Scholar
• Anketell, J. M., & Mriheel, I. Y. (2000). Depositional environment and diagenesis of the Eocene Jdeir Formation, Gabes-Tripoli Basin, western offshore Libya. Journal of Petroleum Geology, 23(4), 425–447. https://doi.org/10.1111/j.1747-5457.2000.tb00495.x
   Web of Science ®Google Scholar
• Arni, P. (1965). L'évolution des Nummulitinae en tant que facteur de modification des dépôts littoraux. Mémoires du BRGM (Paris), 32), 7–20.
   Google Scholar
• Arni, P., & Laterno, E. (1976). Observations paleoecologiques dans l‘Eocene du Gargano (Italie mendionale). Archives Science Geneve, 29, 287–314.
   Google Scholar
• Bard, J. P. (1983). Metamorphism of the obducted island arc: Example of the Kohistan sequence (Pakistan) in the Himalayan collided range. Earth and Planetary Science Letters, 65(1), 133–144. https://doi.org/10.1016/0012-821X(83)90195-4
   Web of Science ®Google Scholar
• Bassi, D. (1998). Coralline algal facies and their palaeoenvironments in the late Eocene of northern Italy (Calcaredi Nago Trento). Facies, 39(1), 179–201. https://doi.org/10.1007/BF02537016
   Google Scholar
• Beavington-Penney, S. J., Wright, V. P., & Racey, A. (2005). Sediment production and dispersal on foraminifera-dominated early Tertiary ramps: The Eocene El Garia Formation, Tunisia. Sedimentology, 52(3), 537–569. https://doi.org/10.1111/j.1365-3091.2005.00709.x
   Web of Science ®Google Scholar
• Berger, S., & Kaever, J. (1992). Dasycladales. An illustrated monograph of a fascinating algal order (p. 247). Thieme.
   Google Scholar
• Bhatia, S., Bhargava, O., Singh, B. P., & Bagi, H. (2013). Sequence stratigraphic framework of the Paleogene succession of the Himalayan foreland basin: A case study from the Shimla Hills. Journal of Palaeontological Society of India, 58(1), 21–38.
   Web of Science ®Google Scholar
• Canudo, J., Keller, G., Molina, E., & Ortiz, N. (1995). Planktic foraminiferal turnover and δ13C isotopes across the Paleocene–Eocene transition at Caravaca and Zumaya, Spain. Palaeogeography, Palaeoclimatology, Palaeoecology, 114(1), 75–100. https://doi.org/10.1016/0031-0182(95)00073-U
   Web of Science ®Google Scholar
• Chassefiere, B., Lundhardt, O., & Levy, A. (1969). Donné es nouvelles sur les cadoules (édifices coquilliers) de la lagunede Thau (Hérault.). Compte Rendu Sommaire des Séances de la Société Géologique de France, 5, 140–142. (in French).
   Google Scholar
• Critelli, S., & Garzanti, E. (1994). Provenance of the Lower Tertiary Murreered beds (Hazara Kashmir Syntaxis, Pakistan) and initial rising of the Himalayas. Sedimentary Geology, 89(3-4), 265–284. https://doi.org/10.1016/0037-0738(94)90097-3
   Web of Science ®Google Scholar
• Cuffey, R. J. (2006). Bryozoan-built reef mounds – The overview from integrating recent studies with previous investigations. In J. Scholz, P. D. Taylor, & N. Vávra (Eds.), Contributions to Bryozoology: A tribute to Ehrhard Voigt (1905–2004). CFS Courier Forschungsinstitut Senckenberg (pp. 35–47).
   Google Scholar
• Davies, L. M., & Pinfold, E. S. (1937). The Eocene beds of the Punjab Salt Range (p. 79). Geological Survey of India. Memoir, 24.
   Google Scholar
• Dunham, R. J. (1962). Classification of carbonate rocks according to depositional texture. In W. E. Ham (Ed.), Classification of carbonate rocks – A symposium (Vol. 1, pp. 108–121). AAPG Memoir. https://doi.org/10.1306/M1357
   Google Scholar
• Eames, E. E. (1951). A contribution to the study of the Eocene in western Pakistan and western India: D. Discussion of the faunas of certain standard sections, and their bearing on the classification and correlation of the Eocene in western Pakistan and western India. Quarterly Journal of the Geological Society, 107(1-4), 173–200. https://doi.org/10.1144/GSL.JGS.1951.107.01-04.08
   Google Scholar
• Fatmi, A. N. (1973). Lithostratigraphic units of the Kohat-Potwar Province, Indus Basin, Pakistan. Geological Survey of Pakistan. Memoir, 16.
   Google Scholar
• Fleury, J. J., Bignot, G., Blondeau, A., & Poignant, A. (1985). Biogeographie de foraminiferes ben hiques tethysiens du Senonien a I’Eocene superieur. Bulletin de la Société Géologique de France, I(5), 757–770. https://doi.org/10.2113/gssgfbull.I.5.757
   Google Scholar
• Flügel, E. (1972). Microproblematikain Dünnschliffen von Trias-Kalken. Mitteilungen der Gesellschaft der Geologie- und Bergbaustudeten. Österreich, 21, 957–988.
   Google Scholar
• Flügel, E. (1982). Microfacies analysis of limestones (p. 633). Springer.
   Google Scholar
• Flügel, E. (1985). Diversity and environments of Permian and Triassic dasycladacean algae. In D. F. Toomey & M. H. Nitecki (Eds.), Paleoalgology (pp. 344–351). Springer. https://doi.org/10.1007/978-3-642-70355-3_28
   Google Scholar
• Flügel, E. (2004). Microfacies of carbonate rocks, analysis, interpretation and application (p. 976). Springer.
   Google Scholar
• Garzanti, E., Baud, A., & Mascle, G. (1987). Sedimentary record of the northward flight of India and its collision with Eurasia (Ladakh Himalaya, India). Geodinamica Acta, 1(4-5), 297–312. https://doi.org/10.1080/09853111.1987.11105147
   Web of Science ®Google Scholar
• Gee, E. R. (1935). The saline series (Early Eocene) of north-western India (abstract). Proceedings of 22nd Indian, Science Congress (p. 207).
   Google Scholar
• Geel, T. (2000). Recognition of stratigraphic sequences in carbonate platform and slope deposits: Empirical models based on microfacies analysis of Paleogene deposits in south-eastern Spain. Palaeogeography, Palaeoclimatology, Palaeoecology, 155(3-4), 211–238. https://doi.org/10.1016/S0031-0182(99)00117-0
   Web of Science ®Google Scholar
• Ghose, B. K. (1977). Paleoecology of the Cenozoic reefal foraminifers and algae – A brief review. Palaeogeography, Palaeoclimatology, Palaeoecology, 22(3), 231–256. https://doi.org/10.1016/0031-0182(77)90030-X
   Web of Science ®Google Scholar
• Gilham, R. F., & Bristow, C. S. (1998). Facies architecture and geometry of a prograding carbonate ramp during the early stages of foreland basin evolution: Lower Eocene sequences, Sierra del Cadı, SE Pyrenees, Spain. In V. P. Wright & T. P. Burchette (Eds.), Carbonate ramps (pp. 181–203). Geological Society of London, Special Publication, 149. https://doi.org/10.1144/GSL.SP.1999.149.01.10
   Google Scholar
• Gingerich, P. D. (1977). A small collection of fossil vertebrates from the Middle Eocene Koldana and Kohat Formations of Punjab (Pakistan). Museum of Paleontology, University of Michigan, Contribution, 24(18), 190–203. https://hdl.handle.net/2027.42/48485
   Google Scholar
• Gingerich, P. D. (2003). Stratigraphic and micropaleontological constraints on the Middle Eocene age of the mammal-bearing Kuldana Formation of Pakistan. Journal of Vertebrate Paleontology, 23(3), 643–651. https://doi.org/10.1671/2409
   Web of Science ®Google Scholar
• Green, O. R., Searle, M. P., Corfield, R. I., & Corfield, R. M. (2008). Cretaceous–Tertiary carbonate platform evolution and the age of the India–Asia collision along the Ladakh Himalaya (Northwest India). The Journal of Geology, 116(4), 331–353. https://doi.org/10.1086/588831
   Web of Science ®Google Scholar
• Hallock, P., & Schlager, W. (1986). Nutrient excess and the demise of coral reefs and carbonate platforms. PALAIOS, 1(4), 389. https://doi.org/10.2307/3514476
   Google Scholar
• Haq, B. U., Hardenbol, J. A., & Vail, P. R. (1987). Chronology of fluctuating sea levels since the Triassic. Science, 235(4793), 1156–1167. http://www.jstor.org/stable/1698241 https://doi.org/10.1126/science.235.4793.1156
   PubMed Web of Science ®Google Scholar
• Henson, F. R. S. (1950). Cretaceous and Tertiary reef formations and associated sediments in Middle East. AAPG Bulletin, 34(2), 215–238. https://doi.org/10.1306/3D933ED2-16B1-11D7-8645000102C1865D
   Web of Science ®Google Scholar
• Herb, R. (1988). Evolution of diversity, paleoenvironments and extinction in large nummulitids. Revue de Paléobiologie, 2, 86–104.
   Google Scholar
• Hewaidy, A. G., Hewaidy, A., Wageeh, M., Ayyad, H., & Gameel, O. (2018). Biostratigraphy, microfacies analysis and sequence stratigraphy of the Miocene successions In Cairo-Suez District, Egypt. Al Azhar Bulletin of Science, 29(1), 39–59.
   Google Scholar
• Hohenegger, J., Yordanova, E., & Hatta, A. (2000). Remarks on west Pacific Nummulitidae (Foraminifera). The Journal of Foraminiferal Research, 30(1), 3–28. https://doi.org/10.2113/0300003
   Web of Science ®Google Scholar
• Hohenegger, J., Yordanova, E., Nakano, Y., & Tatzreiter, F. (1999). Habitats of larger foraminifera on the upper reef slope of Sesoko Island, Okinawa, Japan. Marine Micropaleontology, 36(2-3), 109–168. https://doi.org/10.1016/S0377-8398(98)00030-9
   Web of Science ®Google Scholar
• Höttinger, L. (1960). Recherches sur les Alvéolines du Paléocèneet de l’Eocène. Schweizerische paläeontologische Abhandlungen, 75–76, 1–243.
   Google Scholar
• Höttinger, L. (1973). Selected Paleogene larger foraminifera. In A. Hallam (Ed.), Atlas. Palaeobiogeography (pp. 443–452). Elsevier.
   Google Scholar
• Höttinger, L. (1983). Processes determining the distribution of larger foraminifera in space and time. Utrecht Micropaleontological Bulletins, 30, 239–253.
   Google Scholar
• Jiang, T., Aitchison, J. C., & Wan, X. (2016). The youngest marine deposits preserved in southern Tibet and disappearance of the Tethyan Ocean. Gondwana Research, 32, 64–75. https://doi.org/10.1016/j.gr.2015.01.015
   Web of Science ®Google Scholar
• Kazmi, A. H., & Abassi, I. A. (2008). Stratigraphy and historical geology of Pakistan (p. 524). Department and NCE in Geology, University of Peshawar, Pakistan. ISBN: 978-969-9119.
   Google Scholar
• Langer, M. R., & Hottinger, L. (2000). Biogeography of selected "larger" foraminifera. Micropaleontology, 46(Supplement no. 1), 105–126. http://www.jstor.org/stable/1486184
   Google Scholar
• Levin, H. L. (1957). Micropaleontology of the Oldsmar limestone (Eocene) of Florida. Micropaleontology, 3(2), 137–154. https://doi.org/10.2307/1484194
   Google Scholar
• Li, G. B., & Wan, X. Q. (2003). Eocene microfossils in southern Tibet and the final closing of the Tibetan Tethys. Journal of Stratigraphy, 27(2), 99–108. (in Chinese with English abstract).
   Google Scholar
• Loucks, R. G., Moody, R. T. J., Bellis, J. K., & Brown, A. A. (1998). Regional depositional setting and pore network systems of the El Garia Formation (Metlaoui Group, Lower Eocene), offshore Tunisia. In. D. S. MacGregor, R. T. J. Moody, & D. D. Clark-Lowes (Eds.), Petroleum geology of North Africa (pp. 355–374). Geological Society of London, Special Publication, 132. https://doi.org/10.1144/GSL.SP.1998.132.01.20
   Google Scholar
• Luterbacher, H. (1998). Sequence stratigraphy and the limitations of biostratigraphy in the marine Paleogenestrata of the Tremp Basin (central part of the southern Pyrenean foreland basin, Spain). In P. C. de Graciansky, J. Hardenbol, T. Jacquin, & P. R. Vail (Eds.), Mesozoic and cenozoic sequence stratigraphy of European basins (pp. 303–309). Society for Sedimentary Geology, Special Publication 60.
   Google Scholar
• Malecki, J. (1973). Bathysiphons from the Eocene of the Carpathian flysch, Poland. Acta Palaeontologica Polonica, 18(2) (XVIII), 77–90.
   Google Scholar
• McDougall, J. W., Hussain, A., & Yeats, R. S. (1993). The Main Boundary Thrust and propagation of deformation into the foreland fold-and-thrust belt in northern Pakistan near the Indus River. Geological Society, London, Special Publications, 74(1), 581–588. https://doi.org/10.1144/GSL.SP.1993.074.01.38
   Google Scholar
• Meissner, C. R., Master, J. M., Rashid, M. A., Hussain, M. (1968). Stratigraphy of the Kohat quadrangle (U.S.G.S., Project Report PK-20), 1–86. https://pubs.usgs.gov/pp/0716d/report.pdf
   Google Scholar
• Meissner, C. R., Master, J. M., Rashid, M. A., & Hussain, M. (1974). Stratigraphy of the Kohat quadrangle, Pakistan (U.S.G.S. Professional Paper 716-D), 1–30. https://doi.org/10.3133/pp716D
   Google Scholar
• Meissner, C. R., & Rahman, H. (1973). Distribution, thickness and lithology of Paleocene rocks in Pakistan (U.S.G.S. Professional Paper 716-E). https://pubs.usgs.gov/pp/0716e/report.pdf
   Google Scholar
• Miller, K. G., Rufolo, S., Sugarman, P. J., Pekar, S. F., Browning, J. V., Gwynn, D. W. (1997). Early to middle Miocene sequences, systems tracts, and benthic foraminiferal biofacies. In K. G. Miller & S. W. Snyder (Eds.), Proceedings of the Ocean Drilling Program, Scientific results (Vol. 150X, pp. 169–186). Ocean Drilling Program. https://doi.org/10.2973/odp.proc.sr.150X.313.1997
   Google Scholar
• Molnar, P., & Tapponnier, P. (1975). Cenozoic tectonics of Asia: Effects of a continental collision. Science, 189(4201), 419–426. https://doi.org/10.1126/science.189.4201.419
   PubMed Web of Science ®Google Scholar
• Murray, J. W. (1976). A method of determining proximity of marginal seas to an ocean. Marine Geology, 22(2), 103–119. https://doi.org/10.1016/0025-3227(76)90033-5
   Web of Science ®Google Scholar
• Nagappa, Y. (1959). Foraminiferal biostratigraphy of the Cretaceous–Eocene succession in the India–Pakistan, Burma region. Micropaleontology, 5(2), 145–192. https://doi.org/10.2307/1484208
   Google Scholar
• Najman, Y., Appel, E., Boudagher-Fadel, M., Bown, P., Carter, A., Garzanti, E., Godin, L., Han, J., Liebke, U., Oliver, G., Parrish, R., & Vezzoli, G. (2010). Timing of India–Asia collision: Geological, biostratigraphic, and palaeomagnetic constraints. Journal of Geophysical Research: Solid Earth, 115(B12), B12416. https://doi.org/10.1029/2010JB007673
   Google Scholar
• Najman, Y., & Garzanti, E. (2000). Reconstructing early Himalayan tectonic evolution and paleogeography from Tertiary foreland basin sedimentary rocks, northern India. Geological Society of America Bulletin, 112(3), 435–449. https://doi.org/10.1130/0016-7606(2000)112%3c0435:REHTEA%3e2.3.CO;2
   Web of Science ®Google Scholar
• Parker, F. L. (1971). Distribution of Planktonic. In The Micropalaeontology of Oceans: Proceedings of the Symposium Held in Cambridge from 10 to 17 September 1967 under the Title ‘Micropalaeontology of Marine Bottom Sediments’ (p. 289). Cambridge University Press.
   Google Scholar
• Pascoe, E. H. (1963). A manual of the geology of India and Burma (Vol. 3). Geologic Survey of India.
   Google Scholar
• Patriat, P., & Achache, J. (1984). India–Eurasia collision chronology has implications for crustal shortening and driving mechanism of plates. Nature, 311(5987), 615–621. https://doi.org/10.1038/311615a0
   Web of Science ®Google Scholar
• Pivnik, D. A., & Wells, N. A. (1996). The transition from Tethys to the Himalaya as recorded in northwest Pakistan. Geological Society of America Bulletin, 108(10), 1295–1313. https://doi.org/10.1130/0016-7606(1996)108<1295:TTFTTT>2.3.CO;2
   Google Scholar
• Racey, A. (1994). Biostratigraphy and palaeobiogeographic significance of Tertiary nummulitids (foraminifera) from northern Oman. In M. D. Simmons (Ed.), Micropalaeontology and hydrocarbon exploration in the Middle East (pp. 343–370). Chapman & Hall.
   Google Scholar
• Racey, A. (1995). Lithostratigraphy and larger foraminiferal (nummulitid) biostratigraphy of the Tertiary of northern Oman. Micropaleontology, 41, 1–123. https://doi.org/10.2307/1485849
   Web of Science ®Google Scholar
• Racey, A. (2001). A review of Eocene nummulite accumulations: Structure, formation and reservoir potential. Journal of Petroleum Geology, 24(1), 79–100. https://doi.org/10.1111/j.1747-5457.2001.tb00662.x
   Web of Science ®Google Scholar
• Read, J. F. (1985). Carbonate platform facies models. American Association of Petroleum Geologists Bulletin, 69, 1–21.
   Web of Science ®Google Scholar
• Reichel, M. (1964). Alveolinidae. In R. C. Moore (Ed.), Treatise on invertebrate paleontology, Part C. Protista (Vol. 2, pp. 503–510). University of Kansas Press.
   Google Scholar
• Reiss, Z., & Hottinger, L. (1984). The Gulf of Aqaba: Ecological micropaleontology (p. 354). Springer. https://doi.org/10.1007/978-3-642-69787-6
   Google Scholar
• Renema, W., & Troelstra, S. R. (2001). Larger foraminifera distribution on a mesotrophic carbonate shelf in SW Sulawesi (Indonesia). Palaeogeography, Palaeoclimatology, Palaeoecology, 175(1-4), 125–146. https://doi.org/10.1016/S0031-0182(01)00389-3
   Web of Science ®Google Scholar
• Roohi, G., & Baqri, R. S. H. (2004). The importance of Nummulites and Assilina in the correlation of middle and upper Eocene rocks of Pakistan. Abstract Volume, 19th Himalaya–Karakoram–Tibet Workshop.
   Google Scholar
• Rowley, D. B. (1998). Minimum age of initiation of collision between India and Asia north of Everest based on the subsidence history of the Zhepure Mountain section. The Journal of Geology, 106(2), 220–235. https://doi.org/10.1086/516018
   Web of Science ®Google Scholar
• Sameeni, S. J. (1998). Alveolinid biostratigraphy of the Kohat Formation, northern Pakistan. Geological Society of America Bulletin, 74, 93–114.
   Google Scholar
• Sartorio, D., & Venturini, S. (1988). Southern Tethys biofacies. AGIP.
   Google Scholar
• Schaub, H. (1981). Nummulites et Assilines de la Téthys paléogène: Taxinomie, phylogenèse et biostratigraphie. Schweizerische Paläontologische Abhandlungen, 104, 1–236.
   Google Scholar
• Scholle, P., & Ulmer-Scholle, D. (2003). A color guide to the petrography of carbonate rocks: Grains, textures, porosity, diagenesis (Vol. 77). American Association of Petroleum Geologists, Memoir.
   Google Scholar
• Searle, M. P., Windley, B. F., Coward, M. P., Cooper, D. J. W., Rex, A. J., Rex, D., Tingdong, L. I., Xuchang, X., Jan, M. Q., Thakur, V. C., & Kumar, S. (1987). The closing of Tethys and the tectonics of the Himalaya. Geological Society of America Bulletin, 98(6), 678–701. https://doi.org/10.1130/0016-7606(1987)98<678:TCOTAT>2.0.CO;2
   Web of Science ®Google Scholar
• Sercombe, W. J., Pivnik, D. A., Wilson, W. P., Albertin, M. L., Beck, R. A., & Stratton, M. A. (1998). Wrench faulting in the northern Pakistan foreland: Rethinking a deformed belt. American Association of Petroleum Geologists Bulletin, 82, 2003–2030.
   Web of Science ®Google Scholar
• Serra-Kiel, J., Hottinger, L., Caus, E., Drobne, K., Fernandez, C., Jauhri, A. K., Less, G., Pavlovec, R., Pignatti, J., Samso, J. M., Schaub, H., Sirel, E., Strougo, A., Tambareau, Y., Tosquella, Y., & Zakrevskaya, E. (1998). Larger foraminiferal biostratigraphy of the Tethyan Paleocene and Eocene. Bulletin de la Societe Geologique de France, 169, 281–299.
   Web of Science ®Google Scholar
• Shah, S. M. I. (1977). Stratigraphy of Pakistan (Vol. 12, p. 137). Geological Survey of Pakistan Memoir.
   Google Scholar
• Shahin, A. (2001). Contribution to the knowledge of the Early Cretaceous foraminiferal assemblages, their paleoecology and paleogeography in the northern Sinai, Egypt. Neues Jahrbuch für Geologie und Paläontologie – Abhandlungen, 221(3), 397–440. https://doi.org/10.1127/njgpa/221/2001/397
   Web of Science ®Google Scholar
• Sinclair, H. D., Sayer, Z. R., & Tucker, M. E. (1998). Carbonate sedimentation during early foreland basin subsidence: The Eocene succession of the French Alps. Geological Society, London, Special Publications, 149(1), 205–227. https://doi.org/10.1144/GSL.SP.1999.149.01.11
   Google Scholar
• Tahirkheli, R. A. K., Mattauer, M., Proust, F., & Tapponnier, P. (1979). The India–Eurasia suture zone in the northern Pakistan: Synthesis and interpretation of recent data at plate scale. In A. Farah & K. A. DeJong (Eds.), Geodynamics of Pakistan (pp. 125–130). Geological Survey of Pakistan.
   Google Scholar
• Tanoli, S. K., Abbasi, I. A., Riaz, M., Rehman, O., Iqbal, H., & Akhtar, M. K. (1993). Sedimentology of the Eocene sequence in the Kohat Basin. A collaborative research project between University of Peshawar and OGDCL.
   Google Scholar
• Tucker, M. E., & Wright, V. P. (1990). Carbonate sedimentology (p. 482). Blackwell Science.
   Google Scholar
• van Hinsbergen, D. J., Lippert, P. C., Dupont-Nivet, G., McQuarrie, N., Doubrovine, P. V., Spakman, W., & Torsvik, T. H. (2012). Greater India Basin hypothesis and a two-stage Cenozoic collision between India and Asia. Proceedings of the National Academy of Sciences of the United States of America, 109(20), 7659–7664. https://doi.org/10.1073/pnas.1117262109
   PubMed Web of Science ®Google Scholar
• Van Hinte, J. E. (1978). Geohistory analysis – Application of micropaleontology to exploration geology. The American Association of Petroleum Geologists Bulletin, 62, 201–222. https://doi.org/10.1306/C1EA4815-16C9-11D7-8645000102C1865D
   Web of Science ®Google Scholar
• Wadood, B., Khan, S., Li, H., Wadood, J., Ahmad, S., & Khan, A. (2021a). The Middle Permian (Capitanian) carbonate platform evolution and stratigraphic architecture of a Neo‐Tethys rim basin, Central Pakistan. Geological Journal, 56(8), 4080–4101. https://doi.org/10.1002/gj.4155
   Web of Science ®Google Scholar
• Wang, C. S., Li, X. H., Hu, X. M., & Jansa, L. F. (2002). Latest marine horizon north of Qomolangma (Mt Everest): Implications for closure of Tethys seaway and collision tectonics. Terra Nova, 14(2), 114–120. https://doi.org/10.1046/j.1365-3121.2002.00399.x
   Web of Science ®Google Scholar
• Wells, N. A. (1984). Marine and continental sedimentation in the early Cenozoic of Kohat basin and north-western Indo-Pakistan [Unpublished PhD dissertation]. University of Michigan (p. 465).
   Google Scholar
• Wilson, J. L. (1975). Carbonate facies in geologic history. Springer Science.
   Google Scholar