Structural Evolution of the Kohat and Potwar Fold and Thrust Belts of Pakistan

Total Page:16

File Type:pdf, Size:1020Kb

Structural Evolution of the Kohat and Potwar Fold and Thrust Belts of Pakistan Structural Evolution of the Kohat and Potwar Fold and Thrust Belts of Pakistan Dissertation Von Humaad Ghani zur Erlangung des akademischen Grades DOCTOR RERUM NATURALIUM »DR. RER. NAT.« in der Wissenschaftsdisziplin Geologie eingereicht an der Mathematisch-Naturwissenschaftlichen Fakultät der Universität Potsdam Potsdam, im June 2019 Datum der Disputation: 20.11. 2019 This work is licensed under a Creative Commons License: Attribution – Non Commercial 4.0 International. This does not apply to quoted content from other authors. To view a copy of this license visit https://creativecommons.org/licenses/by-nc/4.0/ Supervisors apl Prof. Edward Sobel Dr Gerold Zeilinger Institute of Geosciences, University of Potsdam, Germany Referees 1: Dr Gerold Zeilinger Institute of Geosciences, University of Potsdam, Germany 2: Prof. Delores Robinson Department of Geological Sciences, University of Alabama, USA 3: Prof. Peter van der Beek ISTerre Université Grenoble Alpes, France Published online at the Institutional Repository of the University of Potsdam: https://doi.org/10.25932/publishup-44077 https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-440775 To my father who left, when I started to understand him Table of Contents Abstract………………………………………….………………………………………...i Zussamenfassung ……………………………………………………………………… iii Preface……………………………………………………………………………………vi Acknowledgments……………………………………………………………………....vii Chapter 1 …………………………………………………………………………………1 Introduction 1.1 Research statement.……………………………………………………………………1 1.2 Aim and objectives of the research………………………………………………........3 1.3 Research methods…...………………………………………………….……….…….3 1.4 Significance of the research…………………………………….……………………..4 1.5 Thesis outline………………………………………………………………………….5 Chapter 2……………………………………………………………………………..5 Chapter 3…………………………………………………………………………......5 Chapter 4…………………………………………………………………………......6 Chapter 5…………………………………………………………………………......6 Chapter 6…………………………………………………………………………......7 Chapter 2………………………………………………………………………………….8 Tectonic framework of northwestern Pakistan 2.1 Hindukush and Karakoram……………………………………………………………8 2.2 Kohistan Arc .........…………………………………………………………………...8 2.3 Himalaya………………………………………………………………………………9 2.3.1 Western Hinterland (metamorphic zone)……………………………………….9 2.3.2 Nanga Parbat Syntaxis………………………………………………………….9 2.3.3 Lesser Himalaya…...………………………………………………………….10 2.3.4 Subhimalaya and Hazara Syntaxis...………………………………………….10 2.4 Himalayan western axial fold and thrust belt..………………………………………11 2.5 Development of the Himalayan fold and thrust belt..……………………………….11 Chapter 3………………………………………………………………………………...13 Structural variation within the Himalayan fold and thrust belt: A case study from the Kohat-Potwar fold thrust belt of Pakistan Abstract……………………………………………………………………………….….13 3.1 Introduction…………………………………………………………………………..13 3.2 Tectonic framework and previous structural interpretations…………………………15 3.3 Stratigraphy and décollements……………………………………………………….18 3.4 Structural style of KP-FTB...………………………………………………………...22 3.4.1 Kohat- Surghar………………………………………………………………..23 3.4.1.1 Seismic profiles...……………………………………………....23 3.4.1.2 Cross-sections…………………………………………………..23 3.4.1.3 Restored sections……………………………………………….25 3.4.2 Potwar, Salt Range and Kalabagh fault zone……………………………………..27 3.4.2.1 Seismic profiles………………………………...………………27 3.4.2.2 Cross-sections…………………………………………………..29 3.4.2.3 Restored sections……………………………………………….30 3.5 Discussion………………………………………………………………...………….31 3.6 Conclusions…………………………………………………………………………..39 Acknowledgments.……………………………………………………………………….39 Chapter 4………………………………………………………………………………...40 Paleozoic to Pliocene tectonic evolution of the Salt Range constrained by low temperature thermochronology Abstract……………………………………………………………………….………….40 4.1 Introduction…………………………………………………………………………..40 4.2 Tectonic framework and stratigraphy…………...…………………………………...41 4.3 Thermochronologic data………………………………………………...…………...42 4.4 Thermal modelling…………………………………………………………………...43 4.5 Discussion and conclusions…………………………………………………………..46 4.5.1 Pre-Himalayan basin history…………………………………………………..46 4.5.2 Development of the Salt Range……………………………………………….47 Acknowledgments……………………………………………………………………......49 Chapter 5………………………………………………………………………………...50 Structural evolution of the Kohat fold and thrust belt, Pakistan Abstract………………………………………………………………….……………….50 5.1 Introduction…………………………………………………………………………..50 5.2 Tectonic framework and stratigraphy.………………………………………………..51 5.3 Apatite low temperature thermochronology…………………………………….……55 5.3.1 Sampling and mineral separation…………………………………………...…55 5.3.2 Analytical methods…………………………………………………………....55 5.3.2.1 U-Th-Sm/He dating (AHe)……………………………………..55 5.3.2.2 Apatite Fission Track dating (AFT)………………………...….56 5.3.3 Results……………….………………………………………………………...56 5.4 Thermal modelling……………………………………………………...……………58 5.5 Balanced cross-section...……………………………………………………………..61 5.6 Discussion…………………………………………………………………...……….63 5.6.1 Sequential structural evolution of Kohat from the MBT to the SGT………....63 5.6.2 Early accretion of the foreland: implications for the Trans Indus Ranges……67 5.6.2.1 Burial and exhumation mechanisms in the Surghar Ranges…...67 5.6.2.2 Development of the Surghar and Khisor Ranges…………..…..68 5.6.3 Thick vs. thin skinned structures……..……………………………………….70 5.7 Conclusions……………………………………………………………………….….71 Acknowledgments……………………………………..……………………………….…71 Chapter 6……………………………………………………………................................72 Synthesis and conclusions 6.1 Pre-Himalayan history of the Salt Range and the adjoining areas……………………72 6.2 Development of the Main Boundary Thrust (MBT)………………………………….73 6.3 Temporal evolution of the structural style and exhumation in the Kohat and Potwar..74 6.4 Spatiotemporal development of the Kohat and Potwar range fronts…………..……...75 6.5 Comparative shortening in the Kohat, Potwar and transfer zone kinematics…............76 6.6 Conclusions……………………………………………………………………………77 6.7 Recommendations for future work……………………...………………………….....78 References………………………………………………………………………………...80 Appendix 1 (Chapter 4).….....…………………………………………...………………...91 1) Section SM 4.1. Sample location and collection strategy………………………….....91 2) Section SM 4.2. Analytical methods……………………………...…………………..94 a) Mineral Separation……………………………………………………………….94 b) Apatite (U-Th-Sm)/He methods and data analysis………………………….……94 c) AFT dating methods and data analysis………………………..…………………96 3) Section SM 4.3. Thermal history modeling………………………………...……….102 4) References…………………………………………………………………………...112 Appendix 2 (Chapter 5)..……………………………………………………………........115 1) Section SM 5.1. Sample locations and characteristics………………...…………….115 2) Section SM 5.2. Low temperature thermochronology data………………………….117 List of Figures Chapter 1 Figure 1.1. Regional tectonic map of the Himalaya and surrounding regions (modified after Beck et al. (1995); Badshah et al. (2000); DiPietro and Pogue, (2004)……………………..….5 Chapter 2 Figure 2.1. Regional tectonic map of the Himalaya and surrounding regions. The inset shows the geographic location………………………………………………………………………..12 Chapter 3 Figure 3.1. Generalized tectonic map of northern Pakistan, showing major geological features………………………………………………………..……………………………….15 Figure 3.2. Evolutionary models of the Kohat and Potwar…………………………………….17 Figure 3.3. Geological map of the study area revised after Meissner et al. (1974) and Gee (1980)…………………………………..………………………………………………….......20 Figure 3.4. Stratigraphic column and correlation chart showing north to south thickness variations of different stratigraphic packages……………………............................................21 Figure 3.5. a) Un-interpreted seismic profiles from the Kohat. b) Interpreted seismic profiles………………………………………………………………………...........................24 Figure 3.6. Cross sections traversing the Kohat (see Figure. 3.3 for location of sections) … .26 Figure 3.7. a) Un-interpreted seismic profiles from the Potwar and the Kalabagh re- entrant…………………………………………………..…………………………………… 28 Figure 3.8. Cross sections through the Potwar, Kalabagh Fault Zone and the Kohat………. ..31 Figure 3.9. Proposed sequential structural evolution within the Kohat………………………..36 Figure 3.10. Field photographs of the Kalabagh Fault Zone. a) Salt diapir in the Molasse sequence. b) KF1 fault shows dextral shear and normal slip movement………………………37 Figure 3.11. Deformed and restored model of the KP-FTB……………………………………37 Figure 3.12. Sketch to show the sequence of thrusting that shaped the Kohat Potwar range front…………………………………………………………………………………………....38 Figure 3.13. 3-D diagram of the KP-FTB illustrating two possible geometries for the basal decollement and the basement normal fault and how these could influence the deflection of the range front……………………………………………………………………………………..38 Chapter 4 Figure 4.1. Structural map of Salt Range and surrounding regions. The inset shows Pakistan and neighboring countries (modified after Gee, (1980); Ghani et al., (2018))……………………...41 Figure 4.2. Geological block diagram showing geometry of the stratigraphic wedge in the Salt Range………………………………………………………………………………………….43 Figure 4.3. QTQt thermal model and age - elevation profile for ten Cambrian and Permian samples combined into a single thermal model……………………………………………….45 Figure 4.4. Development of the Salt Range based on MOVE modeling (Ghani et al., 2018) and our new thermochronologic results……………………………………………………………48 Chapter 5 Figure 5.1. Regional tectonic map of northwestern Pakistan and eastern Afghanistan. Inset map in the lower right shows map location…………………………………………………………52
Recommended publications
  • Peshawar High Court, Peshawar Judicial Department Judgment
    JUDGMENT SHEET PESHAWAR HIGH COURT, PESHAWAR JUDICIAL DEPARTMENT C.R No.289-P/2016 JUDGMENT Date of hearing…………30.10.2018....…………….. Petitioner: (Provincial Housing Authority through its Director General): By Mr. Amir Javed, Advocate. Respondent: No.1, Wazir Khan, by Mr. Tariq Khan Hoti, Advocate. Respondent No.4, Maqsad Ali, Girdawar Circle, Kohat in person. Respondent No.5, Farid Khan, Patwari Halqa Jarma, Kohat in person. **** QALANDAR ALI KHAN, J.- This civil revision by Provincial Housing Authority through its Director General (petitioner) is directed against judgments/orders/decrees dated 24.02.2016 by Additional District Judge-IV, Kohat, and also that of the Civil Judge-XI, Kohat, dated 06.09.2014, whereby decree of the latter Court dated 06.09.2014 was maintained by the former/appellate Court; and appeal of the petitioner dismissed vide impugned judgment and decree dated 24.02.2016. 2. The background, forming basis of the instant revision petition, briefly stated, is that originally the Provincial Government was recorded as owner; and Deputy Commissioner, Kohat, in Possession of the 2 land measuring 219 Kanal in Khasra No.1/1122/71 of village Jarma, according to the available record of owners from the year 2003/04. A total of 300 Kanal land, including the said land, was transferred from the Provincial Government to the Prime Minister National Housing Scheme Authority, vide Mutation No.1033 attested on 22.12.1999; but re-transferred to the Provincial Government from the Pakistan Housing Authority, Works Division, Kohat, vide Mutation No.1062 attested on 28.07.2000. The entire land measuring 300 Kanal , including the land in question measuring 219 Kanal (Banjar Jadeed) was transferred by the Provincial Government to the Provincial Housing Authority) Kohat i.e.
    [Show full text]
  • Updated Stratigraphy and Mineral Potential of Sulaiman Basin, Pakistan
    Sindh Univ. Res. Jour. (Sci. Ser.) Vol.42 (2) 39-66 (2010) SURJ UPDATED STRATIGRAPHY AND MINERAL POTENTIAL OF SULAIMAN BASIN, PAKISTAN M. Sadiq Malkani Paleontology and Stratigraphy Branch, Geological Survey of Pakistan, Sariab Road, Quetta, Pakistan Abstract Sulaiman (Middle Indus) Basin represents Mesozoic and Cainozoic strata and have deposits of sedimentary minerals with radioactive and fuel minerals. The new coal deposits and showings, celestite, barite, fluorite, huge gypsum deposits, marble (limestone), silica sand, glauconitic and hematitic sandstone (iron and potash), clays, construction stone are being added here. Sulaiman Basin was previously ignored for updating of stratigraphy and economic mineral potential. Here most of known information on Sulaiman Basin is compiled and presented along with new economic deposits. Keywords: Stratigraphy, Mineral deposits, Sulaiman Basin, Middle Indus Basin, Pakistan. 1. Introduction metamorphic and sedimentary rocks. The study area is The Indus Basin which is a part of located in the central part of Pakistan (Fig.1a). Gondwanan lands (Southern Earth) is separated by an Previously, the Sulaiman Basin has received little Axial Belt (Suture Zone) from the Balochistan and attention, but this paper will add insights on updated Northern areas of Tethyan and Laurasian domains stratigraphy and new mineral discoveries. (northern earth). The Indus Basin (situated in the North-western part of Indo-Pakistan subcontinent) is 2. Materials and Methods located in the central and eastern part of Pakistan and The materials belong to collected field data, further subdivided in to upper (Kohat and Potwar), during many field seasons like lithology, structure, middle (Sulaiman) and Lower (Kirthar) basins. The stratigraphy and mineral commodities (Figs.
    [Show full text]
  • Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F
    HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 16 Number 1 Himalayan Research Bulletin No. 1 & Article 17 2 1996 Book review of 'Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F. Shroder, Jr. (ed.) Daniel D. Schelling University of Utah Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Schelling, Daniel D.. 1996. Book review of 'Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F. Shroder, Jr. (ed.). HIMALAYA 16(1). Available at: https://digitalcommons.macalester.edu/himalaya/vol16/iss1/17 This Book Review is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. William Fisher Harvard University Himalaya to the Sea: Geology, Geomorphology and the Quaternary. Edited by John F. Shroder, Jr. London, Routledge, 1993. Pp. xxvii + 429. $130.00 Located along the northwestern sector of the within the Himalayan region and South Asia (on which Himalayan continental-collision belt, the Kirthar­ many volumes have been published in recent years), and Sulaiman transform plate-boundary, and the eastern therefore the collection of papers in this volume will be sector of the Makran oceanic-subduction zone, Pakistan of interest to earth scientists working in a large number is one of the most tectonically active regions in the of tectonic, sedimentological and geomorphological world.
    [Show full text]
  • Geology of the Southern Gandghar Range and Kherimar Hills, Northern Pakistan
    AN ABSTRACT OF THE THESIS OF Michael D. Hylland for the degree of Master of Science in Geology presented on May 3. 1990 Title: Geology of the Southern Gandghar Range and Kherimar Hills. Northern Pakistan Abstract approved: RobeS. Yeats The Gandghar Range and Kherimar Hills, located in the Hill Ranges of northern Pakistan, contain rocks that are transitional between unmetarnorphosed foreland-basin strata to the south and high-grade metamorphic and plutonic rocks to the north. The southern Gandghar Range is composed of a succession of marine strata of probable Proterozoic age, consisting of a thick basal argillaceous sequence (Manki Formation) overlain by algal limestone and shale (Shahkot, Utch Khattak, and Shekhai formations). These strata are intruded by diabase dikes and sills that may correlate with the Panjal Volcanics. Southern Gandghar Range strata occur in two structural blocks juxtaposed along the Baghdarra fault. The hanging wall consists entirely of isoclinally-folded Manki Formation, whereas the footwall consists of the complete Manki-Shekhai succession which has been deformed into tight, northeast-plunging, generally southeast (foreland) verging disharmonic folds. Phyllite near the Baghdarra fault displays kink bands, a poorly-developed S-C fabric, and asymmetric deformation of foliation around garnet porphyroblasts. These features are consistent with conditions of dextral shear, indicating reverse-slip displacement along the fault. South of the Gandghar Range, the Panjal fault brings the Gandghar Range succession over the Kherimar Hills succession, which is composed of a basal Precambrian arenaceous sequence (Hazara Formation) unconformably overlain by Jurassic limestone (Samana Suk Formation) which in turn is unconformably overlain by Paleogene marine strata (Lockhart Limestone and Patala Formation).
    [Show full text]
  • A Comparative Study of Directly Selected, In-Service Promoted and Online Selected Subject Specialists Regarding Teaching Effectiveness in Kohat Division, Pakistan
    Journal of Education and Practice www.iiste.org ISSN 2222-1735 (Paper) ISSN 2222-288X (Online) Vol.6, No.10, 2015 A Comparative Study of Directly Selected, In-Service Promoted and Online Selected Subject Specialists Regarding Teaching Effectiveness in Kohat Division, Pakistan Qaiser Suleman PhD (Education) Scholar, Institute of Education & Research, Kohat University of Science & Technology Kohat, Khyber Pakhtunkhwa, (Pakistan) Email: [email protected] Rizwana Gul M.Phil (Education) Scholar, Institute of Education & Research, Kohat University of Science & Technology Kohat, Khyber Pakhtunkhwa, (Pakistan) Abstract The main objective of the study was to compare the teaching effectiveness of directly selected, in-service promoted and online selected subject specialists teaching at higher secondary school level in Kohat Division, Pakistan. The target population of the study was the higher secondary school students in Kohat Division, Pakistan. A sample of 600 students randomly selected from 10 out of 20 higher secondary schools in Kohat Division was used in this study. The design of this research study was survey. A self-developed structured questionnaire was used a research instrument for data collection. Statistical tools i.e., mean, standard deviation, ANOVA and Post-hoc t-tests were used. After statistical analysis, it was concluded that the teaching performance of the directly selected subject specialists was highly appreciable and excellent. On the other hand, teaching performance of in-service promoted subject specialists was found satisfactory while teaching performance of online selected subject specialists was poor and unsatisfactory. Based on findings, it was recommended that at least 75% of the total subject specialists should be recruited through Khyber Pakhtunkhwa Public Service Commission only.
    [Show full text]
  • EVALUATION REPORT (As Ner Llule 35 of Pl' Rules.2004)
    EVALUATION REPORT (As ner llule 35 of Pl' Rules.2004) l. Nameof ProcuringAgency: NationalHighway Authority 2. Methodof Pfocurement: SinqleStage Two EnvelopeProcedure 3, Titleof Procurement: Dualizationand Improvementof Pindigheb-Jand-KohatRoad qUpgradalioniDLralization of Motorway Link frorn Kohatvia Jand).Package -l: Pindigheb- Khushal Garh, Length 34.560 Km 4. Tendellnquiry No.: 21491-01) 5. PPRARef. No. (TSE): TS3?1403E 6. Date& Timeof Bid Closing: 07"'Ausust2017 at 1400hours local time 1. Date& Tirneof Bid Opening: 07'nAuetst 2017 at 1430hours localtime 8. No. of BidsReceived: Seventeen(17) Criteriafor Bid Evaluation: Cliteria olBid Evaluationis attachedat Annex-L 10. Detailsof Bid(s) Evalualion: As below Rule / Regulation/ SBD* / Tcchllical Financial (if Evaluated Cost Policy / Basisfor Rejection Name of firm (if rpplicrble) (Rs.) / Acceptancers per Rule35 applicable) of PP Rules,2004. PriceBid ACEC.NCC(JV) 5,076,307,t35 * 1" Lowest M/s Qualilied opened t'jriceBid M/s ZKlS-ReLiable(JV) 5,088,602,524 2u'r Qualifiecl oDened PficeBid MisKRC-MIM (JV) 5,204,854,721 3,.I Qudified opened PdceBid M/sSMADB-l ItlL-SEC (JV) 5,225,000,000 Qualified opencd PriceBid KNK (JV) 5,352,t98,013 5'l' M/s Qualifled oDencd PriceBid Calsons(JV) 5,407,378,998.56 6'h IVl/sMaqbool- Qualilied ooened PriceBicl (JV) 5,6'7 5,977 ,386 1'1' M/sESER-SN4C Qualified opened PficaBid M/s KAC-HASAS-RMS 5,890,.r00,635 g'h Qualified oDened PriceBid g'r' NLC 5,900,000,000 M/s QuaLifled oDgned PrioeBid 6,013,944,478.12 l0'r' Vl/sl-WO Qurlilied opcned PliceBid NICI-l(afcon-UJC(JV) 6,ts2,952,340 I l" M/s Qualilied opcncd Dis- PriceBid not PPRARule M/sCR20C-Al Mahreeu (JV) Qualified opened 36(b)(v) Dis- PriceBid not -do- (JV) ]vl/sSCDC-AMC Oualilied opened Dis- PliceBid not -do- JV M/s DES-MAAKSONS Oualilied opencd MA CRCCITBurcau Group Co PriceBid not -do- .lVAbdulLah Khan & Co.
    [Show full text]
  • DHIS Khyber Pakhtunkhwa Rapid Assessment 2013.Pdf
    Rapid Assessment of District Health Information System 2013 2 Rapid Assessment of District Health Information System 2013 Table of Contents Acknowledgement ........................................................................................................................................ 6 Survey Team ................................................................................................................................................. 8 Abbreviations ................................................................................................................................................ 9 1 Introduction and background .............................................................................................................. 10 1.1 Data and Management Information System (MIS) ..................................................................... 10 1.2 Background ................................................................................................................................. 10 1.3 Gaps of HMIS ............................................................................................................................. 11 1.4 District Health Information System (DHIS) ............................................................................... 11 1.5 Role of DHIS in Khyber Pakhtunkhwa ....................................................................................... 11 1.6 Comparison between HMIS and DHIS ......................................................................................
    [Show full text]
  • Seismic Data Interpretation and Fault Mapping in Badin Area, Sindh, Pakistan
    Sindh Univ. Res. Jour. (Sci. Ser.) Vol.46 (2):133-142 (2014) SINDH UNIVERSITY RESEARCH JOURNAL (SCIENCE SERIES) Seismic Data Interpretation and Fault Mapping in Badin Area, Sindh, Pakistan A. MUNIR, S. ASIM++, S. A. BABLANI*, A. A. ASIF** Department of Earth Sciences, Quaid-i-Azam University, Islamabad, Pakistan Received 12th June 2013 and Revised 9th March 2014 Abstract: The purpose of this research is to study structural variations of subsurface using seismic and well log data of Badin area. 2D seismic reflection data of ten lines after correlation with five wells of the area reveal that extensive structural and depositional changes have occurred as a result of major & minor tectonic events. Seismic interpretation confirms Horst & Graben geometry in the studied area. Grabens are main areas for generation of hydrocarbons. Primary structuring is defined by structural style at Middle Sand level. Compensating faults are increased at shallower level (Top Lower Goru) due to variation in rock mechanics and applied forces. The variable throw at different levels describes structural evolution through the geological time. Contour maps in two way time and depth domain show faults having northwest to southeast trend in the studied area. Seismic and well data is used to establish stratigraphic correlations of different wells in Lower Indus Basin and also to elucidate the source of sediments and depositional centers during different geological time periods. Structuring in the area provides basic elements of requirements of petroleum system as proven by number of oil and gas discoveries in the area. Faults act as conduits providing migration pathway from source to reservoir rock and seals in trapping mechanism for hydrocarbons.
    [Show full text]
  • Khyber Pakhtunkhwa FATA Punjab a JK Islamabad FA NA Disputed Area
    Pakistan: Deployment of mobile and static clinics in Khyber Pakhtunkhwa Province as on august 4, 2010 Services of mobile clinics deployed on the KPK province Comp. PHC Referral Provision of Basic Basic Comp Nutrition Kalam Organisation Name District Tehsil Union Council ANC PNC IMNCI Services Services Medicines Lab EmONC EmONC Surveillance FANA A Bahrain Yes Yes Yes Yes Yes Yes N Care International Sw at Bahrain Tirat Yes Yes Yes Yes Yes Yes Disputed Area l Bahrain a FATA Khyber Pakhtunkhwa A Amazai Yes Yes Yes Yes Yes Yes ky an F B M Kaw ga Yes Yes Yes Yes Yes Yes ah r Punjab ain Makhranai Yes Yes Yes Yes Yes Yes Naw agai Yes Yes Yes Yes Yes Yes Gowalairaj Balochistan Ellai Yes Yes Yes Yes Yes Yes Tirat Buner Chamla Tehsil Krapa Yes Yes Yes Yes Yes Yes Bar Thana Sind Bahrain Mankyal Yes Yes Yes Yes Yes Khwazakhela Matta Sebujni Bar Thana Yes Yes Yes Yes Yes Yes Matta Khararai Shin Gow alairaj Yes Yes Yes Yes Yes Yes Swat Kotanai Dherai Yes Yes Shahpur IDEA Sw at Matta Sebujni Malik Khel Yes Yes Jano/chamtalai Concern Worldw ide Kohat Kohat Tehsil Sher Kot Yes Yes Yes Yes Yes Khawazakhela rai Buner Daggar Tehsil Daggar Kabal Charbagh Dhe Dhoda Malik Khel Kohat Kohat Tehsil Urban-4 Shangla Jano/chamtalai Babuzai Khaw azakhela Kotanai Yes Barikot Sori Chagharzai Sw at Khw azakhela Shin Gul Bandai Jarma Yes Yes Yes Yes Yes Yes Yes r a Handicap International Kohat Kohat Tehsil Lachi Rural Yes Yes Yes Yes Yes Yes Yes g g a Batara Batara Yes Yes Yes Yes Yes Yes D ai Ell Gul Bandai Yes Yes Yes Yes Yes Yes Buner Merlin Buner Chagharzai Tehsil
    [Show full text]
  • KT15D00002-Repair Approach Street Dispensary Mirahmad Khel 220,000 220,000 220,000 220,000
    District Project Description BE 2017-18 Final Budget Releases Expenditure KOHAT KT15D00002-Repair approach street dispensary MirAhmad khel 220,000 220,000 220,000 220,000 KOHAT KT15D00003-Const of Toilets, waiting shed andother 740,000 740,000 740,000 740,000 repair/maintenance of BHU Sherkot KOHAT KT15D00004-Pipe Line at BHU LandiKachai, Repair ofroof of RHC 649,000 649,000 649,000 649,000 UstarZai, Repair Work at RHC Usterzai. KOHAT KT15D00005-Maj; repair, w/s and elect, BHU KhaddarKhel 423,892 423,892 423,892 423,892 KOHAT KT15D00006-R&(M) works, const of waiting shed andG/Lat 04 No. 740,000 740,000 740,000 740,000 at RHC Lachi Bala KOHAT KT15D00007-R&(M) at BHU Ali Kach 740,000 740,000 740,000 740,000 KOHAT KT15D00008-Elect, W/S, Sanitary and building repairBHU Dolli 596,291 596,291 596,291 596,291 Banda KOHAT KT15D00009-Prov; of health related equipments andhygienic kits in 740,000 740,000 740,000 - civil hospital Shakardara Urban. Dev; works at civilHospital Shakardara. KOHAT KT15D00010-Solarization at BHU Gabari in U/CShakardara Rural-II. 740,000 740,000 740,000 - KOHAT KT15D00011-Major Repair of buildings and w/s of BHUGabari 740,000 740,000 740,000 740,000 KOHAT KT15D00012-Const;/repair works and S/F of Hand Pumpat BHU 488,122 488,122 488,122 488,122 Surgul KOHAT KT15D00013-Pavement of Dispensary street at U/CUrban III 507,090 507,090 507,090 507,000 KOHAT KT15D00014-Purchase of Hygienic kits,Purchase ofHematology 3,981,535 3,981,535 3,981,535 1,204,000 analyzer, for LMH Kohat, Purchase of Spray Pumps andInsecticides KOHAT KT15D00015-Const:
    [Show full text]
  • Lithofacies, Depositional Environments, and Regional Stratigraphy of the Lower Eocene Ghazij Formation, Balochistan, Pakistan
    U.S. Department of the Interior U.S. Geological Survey Lithofacies, Depositional Environments, and Regional Stratigraphy of the Lower Eocene Ghazij Formation, Balochistan, Pakistan U.S. Geological Survey Professional Paper 1599 Prepared in cooperation with the Geological Survey of Pakistan A Cover. Exposures of the lower Eocene Ghazij Formation along the northeast flank of the Sor Range, Balochistan, Pakistan. Photograph by Stephen B. Roberts. Lithofacies, Depositional Environments, and Regional Stratigraphy of the Lower Eocene Ghazij Formation, Balochistan, Pakistan By Edward A. Johnson, Peter D. Warwick, Stephen B. Roberts, and Intizar H. Khan U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1599 Prepared in cooperation with the Geological Survey of Pakistan UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1999 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Charles G. Groat, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Lithofacies, depositional environments, and regional stratigraphy of the lower Eocene Ghazij Formation, Balochistan, Pakistan / by Edward A. Johnson . .[et al.]. p. cm.—(U.S. Geological Survey professional paper ; 1599) "Prepared in cooperation with the Geological Survey of Pakistan." Includes bibliographical references. 1. Geology, Stratigraphic—Eocene. 2. Geology—Pakistan— Balochistan. 3. Coal—Geology—Pakistan—Balochistan. 4. Ghazij Formation (Pakistan). I. Johnson, Edward A. (Edward Allison), 1940- . II. Series. QE692.2.L58 1999 553.2'4'0954915—dc21 98-3305 ISBN=0-607-89365-6 CIP CONTENTS Abstract..........................................................................................................................
    [Show full text]
  • Redalyc.Geochemistry and Provenance of the Lower Siwaliks
    Geologica Acta: an international earth science journal ISSN: 1695-6133 [email protected] Universitat de Barcelona España Ullah, K.; Arif, M.; Tahir Shah, M. Geochemistry and provenance of the Lower Siwaliks from southwestern Kohat, western Himalayan Foreland Basin, NW Pakistan Geologica Acta: an international earth science journal, vol. 13, núm. 1, marzo, 2015, pp. 45-61 Universitat de Barcelona Barcelona, España Available in: http://www.redalyc.org/articulo.oa?id=50538715003 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Geologica Acta, Vol. 13, Nº 1, March 2015, 45-61 DOI: 10.1344/GeologicaActa2015.13.1.3 Geochemistry and provenance of the Lower Siwaliks from southwestern Kohat, western Himalayan Foreland Basin, NW Pakistan K. ULLAH1 M. ARIF2,3* M. TAHIR SHAH4 1University of Peshawar, National Center of Excellence in Geology P.O. Box No. 734, University Campus, Peshawar 25120, Pakistan. 2 University of Peshawar, Department of Geology Peshawar 25120, Pakistan. 3 CIIT Department of Earth Sciences Abbottabad 22060, Pakistan. 4 University of Peshawar, National Center of Excellence in Geology Peshawar 25120, Pakistan. *Corresponding author: E-mail: [email protected] ABS TRACT Equivalent to the Lower Siwalik Group, the Late Miocene Chinji Formation in Pakistan consists of interbedded in-channel sandstone (SSt) and overbank mudstone (MSt) sequences. Twelve sandstone and sixteen mudstone samples from three different sections of the formation in southwestern Kohat, NW Pakistan were analyzed for major elements and selected trace elements.
    [Show full text]