Microfacies Analysis and its Implications for Depositional Environment of Margala Hill Limestone from Khaira Gali Road Section, North Eastern Hazara, Pakistan

Adabi, M.H., Zohdi, A., Ghabeishavi, A., Amiri-Bakhtiyar, H., 2008. Applications of nummulitids and
other larger benthic foraminifera in depositional environment and sequence stratigraphy: an example
from the Eocene deposits in Zagros Basin, SW Iran. Facies, 54 (4): 499-512.##
Afzal, J., 2011. Evolution of larger benthic foraminifera during the Paleocene-early Eocene interval in
the east Tethys (Indus Basin, Pakistan) (Doctoral dissertation, University of Leicester).##
Afzal, J., Williams, M., Aldridge, R.J., 2009. Revised stratigraphy of the lower Cenozoic succession of
the Greater Indus Basin in Pakistan. Journal of Micropalaeontology, 28 (1): 7-23.##
Ahsan, N., Chaudhry, M.N., 2008. Geology of Hettangian to Middle Eocene Rock of Hazara and
Kashmir Basins, northwest lesser Himalayas, Pakistan. Geological Bulletin of Punjab University, 43:
131-152.##
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.##
Baig, M.S., 1991. Geochronology of pre-Himalayan and Himalayan tectonic events, northwest
Himalaya, Pakistan. Kashmir Journal of Geology, 8 (9): 197.##
Baig, M.S., Lawrence, R.D., Snee, L.W., 1988. Evidence for late Precambrian to early Cambrian
orogeny in northwest Himalaya, Pakistan. Geological Magazine, 125: 83-86.##
Baig, M.S., Snee, L.W., La-Fortune, R.J., 1989. Timing of the Pre-Himalayan organic events in the
Northwestern Himalaya: 40 Ar/39 Ar constraints. Kashmir Journal of Geology 6-7: 29-40.##
BouDagher-Fadel, M.K., 2012. Biostratigraphic and geological significance of planktonic foraminifera
22.##
Chaudhry, M.N., Ahsan, N., Ghazanfar, M., 1998. A Preliminary Account of Sedimentology of Hazara
Basin from Jurassic to Eocene. 13th Himalaya-Karakoram-Tibet Workshop. Geological Bulletin
University of Peshawar, 31: 41-43.##
Cheema, A.H., 2010. Microfacies, Diagenesis and Depositional Environments of Samana Suk
Formation (Middle Jurassic) Carbonates exposed in South East Hazara and Samana Range (Doctoral
dissertation, University of the Punjab).##
Davies, L.M., Pinfold, E.S., 1937. The Eocene Beds of the Punjab Salt Range. Memoirs of the
Geological Survey of India. Palaeontologia Indica, 24: 1-79.##
Davies, L.M., 1927. The Ranikot beds at Thal (north-west frontier provinces of India). Quarterly Journal
of the Geological Society, 83(1-5): 260-290.##
DiPietro, J.A., Pogue, K.R., 2004. Tectonostratigraphic subdivisions of the Himalaya: A view from the
west. Tectonics, 23(5).##
Duppret, L., Dissler, E., Dore, F., Gresselin, F., Gall, J.E., 1990. Cadomian geodynamic evolution of
the northeastern Armorican Massif In: D’Lemos RS et al (eds) The Cadomian Orogeny. Geological
society of London, 115-131 p.##
Flugel, E., 2013. Microfacies of carbonate rocks: analysis, interpretation and application. Springer
Science & Business Media.##
Gansser, A., 1980. The significance of the Himalayan suture zone. Tectonophysics, 62(1-2): 37-52.
Gill, W.D., 1953. Facies and fauna in the Bhadrar beds of the Punjab Salt Range, Pakistan. Journal of
Paleontology, 824-844.##
Hodges, K.V., 2000. Tectonics of the Himalaya and southern Tibet from two perspectives. Geological
Society of America Bulletin, 112(3): 324-350.##
Hottinger, L., 1960, Recherches sur les Alvéolines du Palécène et de l'Eocène.: Schweizerische
Palaeontologische Abhandlungen, 75-76: 1-243.##
Hottinger, L., 1983. Processes determining the distribution of larger foraminifera in space and
time. Utrecht Micropaleontological Bulletins, 30: 239-253.##
Hottinger, L., 2009. The Paleocene and earliest Eocene foraminiferal Family Miscellaneidae: neither
nummulitids nor rotaliids. Carnets de géologie.##
Jagoutz, O., Schmidt, M.W., 2012. The formation and bulk composition of modern juvenile continental
crust: The Kohistan arc. Chemical Geology, 298: 79-96.##
Jauhri, A.K., Misra, P.K., Kishore, S., Singh, S.K., 2006. Larger foraminiferal and calcareous algal
facies in the Lakadong Formation of the South Shillong Plateau, NE India. Journal of the
Palaeontological Society of India, 51(2): 51-61.##
Jouanne, F., Awan, A., Pecher, A., Kausar, A., Mugnier, J.L., Khan, I., Khan, N.A., Van Melle, J., 2014.
Present‐day deformation of northern Pakistan from Salt Ranges to Karakorum Ranges. Journal of
Geophysical Research: Solid Earth, 119(3): 2487-2503##
Kazmi, A.H., Abbasi, I.A., 2008. Stratigraphy and Historical Geology of Pakistan. Dept. &
NCE. Geology, University of Peshawar, Pakistan, 524 p.##
Kazmi, A.H., Jan, M.Q., 1997. Geology and Tectonics of Pakistan: Graphic Publishers, Karachi,
Pakistan.##
Latif, M.A., 1970. Explanatory notes on the geology of southeastern Hazara to accompany the revised
geological map. Jahrbuch der Geologischen Bundesanstalt, Sonderband, 15: 5-20.##
Latif, M.A., 1976. Stratigraphy and micropaleontology of the Galis Group of Hazara,
Pakistan. Geological Bulletin of Punjab University, 13: 1-64.##
Leckie, R.M., 1989. A paleoceanographic model for the early evolutionary history of planktonic
foraminifera. Palaeogeography, Palaeoclimatology, Palaeoecology, 73(1-2): 107-138.##
Nagappa, Y., 1959. Foraminiferal biostratigraphy of the Cretaceous-Eocene succession in the India-
Pakistan-Burma region. Micropaleontology, 5(2): 145-177.##
Nuttall, W.L.F., 1926. The larger foraminifera of the Upper Ranikot Series (Lower Eocene) of Sind,
India. Geological Magazine, 63(3): 112-121.##
Paracha, W., 2004. Kohat plateau with reference to Himalayan tectonic general study. CSEG recorder.
Payros, A., Orue-Etxebarria, X., Pujalte, V., 2006. Covarying sedimentary and biotic fluctuations in
Lower-Middle Eocene Pyrenean deep-sea deposits: Palaeoenvironmental
implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 234(2-4): 258-276.##
Pecher, A., Seeber, L., Guillot, S., Jouanne, F., Kausar, A., Latif, M., Majid, A., Mahéo, G., Mugnier,
J.L., Rolland, Y., Van Der Beek, P., 2008. Stress field evolution in the northwest Himalayan syntaxis,
northern Pakistan. Tectonics, 27(6).##
Racey, A., Simon, J.B.P., 2004. Ecology of extant nummulitids and other larger benthic foraminifera:
applications in palaeoenvironmental analysis. Earth-Science Reviews 67: 219-265.##
Racey, A., 2001. A review of Eocene nummulite accumulations: structure, formation and reservoir
potential. Journal of Petroleum Geology, 24(1): 79-100.##
Schaub, H., 1981. Nummulites at Assilines de la Téthys paléogène: taxinomie, phylogenèse et
biostratigraphie. Atlas I:* Hans Schaub. Birkhäuser.##
Scheibner, C., Speijer, R.P., 2008. Late Paleocene-early Eocene Tethyan carbonate platform
evolution—A response to long-and short-term paleoclimatic change. Earth-Science Reviews, 90(3-
4): 71-102.##
Searle, M.P., Treloar, P.J., 2010. Was Late Cretaceous-Paleocene obduction of ophiolite complexes the
primary cause of crustal thickening and regional metamorphism in the Pakistan
Himalaya?. Geological Society, London, Special Publications, 338(1): 345-359.##
Sengor, A.M.C., Altiner, D., Cin, A., Ustaomer, T., Hsu, K.J., 1988. Origin and assembly of the
Tethyside orogenic collage at the expense of Gondwanaland. In: Audley-Charles MG, Hallam A
(eds) Gondwana and Tethys. Geological Society of London Special Publications 37: 81-119.##
Serra-Kiel, J., Hottinger, L., Caus, E., Drobne, K., Ferrandez, C., Jauhri, A.K., Less, G., Pavlovec, R.,
Pignatti, J., Samso, J.M., Schaub, H., 1998. Larger foraminiferal biostratigraphy of the Tethyan
Paleocene and Eocene. Bulletin de la Société géologique de France, 169(2): 281-299.##
Shah, S.M.I., 2009, Stratigraphy of Pakistan: Memoir Geological Survey of Pakistan, 22: 381.##
Tlig, S., Sahli, S., Er-Raioui, L., Alouani, R., Mzoughi, M., 2010. Depositional environment controls on
petroleum potential of the Eocene in the North of Tunisia. Journal of Petroleum Science and
Engineering, 71(3-4): 91-105.##
Wanamaker Jr, A.D., Hetzinger, S., Halfar, J., 2011. Reconstructing mid-to high-latitude marine climate
and ocean variability using bivalves, coralline algae, and marine sediment cores from the Northern
Hemisphere. Palaeogeography, Palaeoclimatology, Palaeoecology, 302(1-2): 1-9.##
Wilson, J.L., 2012. Carbonate facies in geologic history. Springer Science & Business Media.
Zhang, Q., Willems, H., Ding, L., 2013. Evolution of the Paleocene-Early Eocene larger benthic
foraminifera in the Tethyan Himalaya of Tibet, China. International Journal of Earth
Sciences, 102(5), 1427-1445.##