DOCSLIB.ORG

International Workshop on Tethyan Orogenesis and Metallogeny in Asia and Cooperation Among

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
International Workshop on Tethyan Orogenesis and Metallogeny in Asia and Cooperation Among International Workshop on Tethyan Orogenesis and Metallogeny in Asia and Cooperation among Institutions of Higher Education Extended Abstract Volume Edited by Changqian Ma, Paul T. Robinson and Yunlong He Mafic dykes in Paleo-Tethyan granitoid pluton (East Kunlun, Northern Qinghai-Tibet Plateau) China University of Geosciences 11th - 16th October, 2014 Wuhan, China Organization Structure of Workshop Scientific Committee Chair: Jingsui Yang (China) Co-Chairs: Erdin Bozkurt (Turkey) Jianwei Li (China) Paul T. Robinson (China) Qinglai Feng (China) Hassan Mirnejad (Iran) Olga Sayfulloeva (Tajikistan) Members: Sajjad Ahmed (Pakistan) Roger Mason (China) Jonathan Aitchison (Australia) Lianfu Mei (China) Honghan Chen (China) U.ur Ka.an Tekin (Turkey) Chongpan Chonglakmani (Thailand) Nguyen Van Vuong (Vietnam) Farahnaz Daliran (Germany) Guocan Wang (China) Mohammad Naim Eqrar (Afghanistan) Guoqing Wang (China) Mohammad Hassan Karimpour (Iran) Jiasheng Wang (China) Xinbiao Lv (China) Organizing Committee Chair: Changqian Ma (China) Co-chairs: Qinglai Feng (China) Lailin Sun (China) Hongtao Su (China) Lijun Zhang (China) Members: Myo Min (Myanmar) Mongkol Udchachon (Thailand) Zhenbing She (China) Yunlong He (China) Sihai Wang (China) Hui Wang (China) Dan Wu (China) Sponsors China University of Geosciences (CUG), Wuhan National Natural Science Foundation of China, Beijing State Key Laboratory of Geologcial Processes and Mineral Resources, CUG, Wuhan State Key Laboratory of Continental Tectonics and Dynamics, CAGS, Beijing Contents Basaltic flows in the Laki Range of the Lower Indus Basin, Sindh, Pakistan: evidence for northwestern extension of the Deccan traps .................................................................................. 1 Muhammad Hassan Agheem, Qasim Jan, Sarfraz Hussain Solangi, Amanullah Laghari, Humaira Dars Petrogenesis of Late Carboniferous gabbro east of Misho, Northwest Iran, based on geochemical and Sr–Nd isotopic data ................................................................................................................ 2 Maryam Ahankoub Hydrology of the Himalaya Mountains under a changing climate from historical stream gauge data for selected watersheds in Pakistan ....................................................................................... 6 Zulfiqar Ahmad Review of the geology of gold-bearing quartz veins in the Tethyan orogenic belt- A case study of the Mayum gold deposit, Tibet, SW China ................................................................................... 7 Hafizullah Abba Ahmed, Ismaila V. Haruna, Mukhtar Habib, Jakada Hamza, Mohammed Ishag Mohammed Abdallsamed The importance of field observations in geological investigations: Some stratigraphic constraints on the timing of India-Asia collision ............................................................................................ 8 Jonathan Aitchison Palaeoproductivity and palaeoredox conditions of the HuaiHinLat Formation in Northeastern Thailand ...................................................................................................................................... 10 Boonnarong Arsairai,Akkhapun Wannakomol,QinglaiFeng, Chongpan Chonglakmani Ophiolites: their magmatic evolution and emplacement mechanisms .................................................. 12 Yildirim Dilek Water resources of Afghanistan and their trans-boundary context ....................................................... 14 M.Naim Eqrar Temporal and spatial distribution of major metal deposits in the Eastern Tethyan metallogenic domain: a review ......................................................................................................................... 16 Yuheng Guo, Changqian Ma Assessing the viability of research cooperation for petroleum exploration and production: A case study of the Federal University of Technology (FUT), Minna, Nigeria and CUG, Wuhan, China ........................................................................................................................................... 17 Mukhtar Habib, Yao GuangQing, Congjiao Xie, Hamza Jakada Volcanogenic massive sulfide mineralization in the Kashan-Delijan region, Iran ............................... 21 Fayeq Hashemi, Fardin Mousivand, Mehdi Rezaei-Kahkhaei Stratigraphy and paleontology of marine Permian and Triassic sequences in the Nong Prue district, Kanchanaburi Province, Thailand .................................................................................. 25 Krongkaew Jenjitpaiboon, Chongpan Chonglakmani Paleozoic-Mesozoic magmatism and metallogeny in the Laojunshan district, Yunnan Province, South China ................................................................................................................................. 27 Shaoyong Jiang, Bin Xu, Rong Wang Time constraints on partial melting and deformation of the Himalayan crystalline sequence, Nyalam Tibet: implications for orogenic models ........................................................................ 29 Philippe Hervé Leloup, Gweltaz Mahéo, Alexandre Aubray, Xiaobing Liu, Xiaohan Liu, Jean-Louis Paquette, Nicolas Arnaud I Magmatism and mineralization in the Permian large igneous province in the Tarim Basin, NW China ........................................................................................................................................... 32 Zilong Li, Yinqi Li, Shufeng Yang, Hanlin Chen, Yu Xing, Siyuan Zou Late Permian back-arc basin development in the western Jinshajiang suture zone, Central Qinghai-Tibetan Plateau: evidence from the Yushu mafic-ultramafic rocks .............................. 34 Bin Liu, Changqian Ma, Xin Zhang, Pan Guo, Fuhao Xiong Analysis of the mechanism of faulting and uplift in the Huizhou depression, Pearl River Delta, South China ................................................................................................................................. 37 Hailun Liu Different mantle evolutions between the Paleo-Asian and Paleo-Tethyan domains deduced from Pb isotopic data ........................................................................................................................... 39 Xijun Liu, Wenjiao Xiao, Jifeng Xu, Paterno R Castillo Subduction and oceanic ridges and ophiolite obduction ....................................................................... 43 Roger Mason Crustal assembly of Myanmar: establishing a geo/thermochronological database for magmatism, metamorphism, deformation, and exhumation in central and eastern Myanmar ........................ 46 Myo Min, Lothar Ratschbacher, Eva Enkelmann, Leander Franz, Raymond Jonckheere, Marion Tichomirowa Evaluating the origin of major magmatic iron deposits in Iran (Gol-Gohar, Sanagan and Bafq): constraints from geological, mineralogical and geochemical characteristics ............................. 48 Hassan Mirnejad Volcanogenic massive sulfide Cu-ag mineralization in the Kharturan area, southeast of Shahrood .... 53 Fadin Mousivand Record of tectonic transformation in SW Yunnan: Geochemical and zircon U–Pb geochronological evidence from arc-derived, Late Devonian volcanogenic sediments in the southern Lancangjiang zone ........................................................................................................ 54 Xiaomei Nie, Qinglai Feng Petrography, geochemistry and U-Pb detrital zircon dating of the clastic Phu Khat Formation in the Nakhon Thai region, Thailand: implications for provenance and geotectonic setting .......... 56 Pradit Nulay, Chongpan Chonglakmani, Qinglai Feng Application of geochemical fingerprinting to mineral deposit classification and exploration .............. 58 J. A. Pearce Geochemical and geochronology constraints on the origin of the meta-mafic volcanic rocks in the Tengtiaohe Zone, SW China ....................................................................................................... 62 Xin Qian, Qinglai Feng, Yuejun Wang, Zhibin Zhang Porphyry Cu-Au, Mo and Cu-Mo metallogenic systems in the Qinghai-Tibetan Plateau from subduction and continental collision to transitional settings ....................................................... 63 Kezhang Qin, Guangming Li, Junxing Zhao, Jinxiang Li, Bo Xiao, Lei Chen, Mingjian Cao New perspectives on ophiolite formation: evidence from UHP, highly reduced and crustal minerals in mantle peridotites and podiform chromitites ............................................................ 67 Paul T. Robinson, Jingsui Yang, Fahui Xiong and Xiangzhen Xu Geodynamics of the inner and outer Zagros Ophiolite belt (Iran), inferred from the chemical composition of Cr-spinel in chromitites ...................................................................................... 69 Fatemeh Sepidbar, Hassan Mirnejad Petrography and mineral chemistry of volcanic rocks south of Bardsir (Dahaj-Sarduieh, Iran): evidence for magma mixing ........................................................................................................ 73 Fatemeh Sepidbar, Hassan Mirnejad II Tectonic setting of plagiogranites and gabbros in the Shahre-Babak ophiolitic sequence (Nain- Baft belt), Iran ............................................................................................................................. 77 Fatemeh Sepidbar, Hassan Mirnejad Late Cretaceous intra-plate volcanism in Ceno-Tethys: evidence from the Kazhaba Volcanics, Balochistan, Pakistan .................................................................................................................
Load more

Recommended publications
  • ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh
    ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0016–7800 ISBN 3-85316-02-6 Band 54 S. 385–434 Wien, Oktober 1999 North Gondwana: Mid-Paleozoic Terranes, Stratigraphy and Biota Editors: R. Feist, J.A. Talent & A. Daurer Paleogeographic Implications of a Devonian (Givetian, Lower Varcus Subzone) Rugose Coral Fauna from the Ma’der Basin (Morocco)*) ALAN E.H. PEDDER**) 4 Text-Figures and 11 Plates Morocco Devonian Rugose Corals Paleogeography Biostratigraphy Contents Zusammenfassung ...................................................................................................... 385 Abstract ................................................................................................................. 386 1. Introduction ............................................................................................................. 386 2. Jbel Ou Driss Locality and Fauna ......................................................................................... 386 3. Comparisons with Other Regions ......................................................................................... 387 3. 1. Appalachian Belt, Eastern Americas Realm .......................................................................... 388 3. 2. Northern Spain, Pyrénées and the Vendée ........................................................................... 388 3. 3. Northern Vosges, Saar, Moravia ...................................................................................
    [Show full text]
  • Phosphate Occurrence and Potential in the Region of Afghanistan, Including Parts of China, Iran, Pakistan, Tajikistan, Turkmenistan, and Uzbekistan
    Phosphate Occurrence and Potential in the Region of Afghanistan, Including Parts of China, Iran, Pakistan, Tajikistan, Turkmenistan, and Uzbekistan By G.J. Orris, Pamela Dunlap, and John C. Wallis With a section on geophysics by Jeff Wynn Open-File Report 2015–1121 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2015 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Orris, G.J., Dunlap, Pamela, and Wallis, J.C., 2015, Phosphate occurrence and potential in the region of Afghanistan, including parts of China, Iran, Pakistan, Tajikistan, Turkmenistan, and Uzbekistan, with a section on geophysics by Jeff Wynn: U.S. Geological Survey Open-File Report 2015-1121, 70 p., http://dx.doi.org/10.3133/ofr20151121. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Contents
    [Show full text]
  • 7. Rickards, Wright, Hamedi.Pdf
    Records of the Western AustralIan Museum Supplement No. 58: 103-122 (2000). Late Ordovician and Early Silurian graptolites from southern Iran R.B. Rickardsl, A.J. Wright2 and M.A. HamedP I Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3 EQ, England 1 School of Geosciences, University of Wollongong, Wollongong, N.s.W. 2522, Australia "Department of Geology, Tarbiet Modares University, Tehran, Iran Abstract - Graptolites are described for the first time from the Faraghun mountains (Kuh-e-Faraghun) and the Gahkum mountains (Kuh-e-Gahkum) on the northern edge of the southeast part of the Zagros Mountains, Iran. 38 taxa are recorded, including 4 Ordovician and 34 Silurian species; the latter are the first Silurian graptolites described from Iran. Ashgill (Late Ordovician) graptolite assemblages from Kuh-e-Faraghun include: Persclllptograptlls persculptlls and Orthograptlls amplexicalllis, indicating a persculptlls Biozone age; and Orthograptus amplexicalllis abbreviatlls, indicating the latest Ordovician anceps Biozone. Kuh-e-Faraghun Early Silurian faunas include representatives of the L1andovery leptotheca Biozone; another assemblage, including Monograptlls convollltus and Pselldorthograptlls inopinatlls, indicates the slightly younger L1andovery convollltlls Biozone. Graptolites from Kuh-e-Gahkum comprise a rich Stimlllograptlls sedgwickii assemblage, indicating a slightly higher L1andovery level again (sedgwickii Biozone); a convollltlls Biozone fauna is also probably represented in our collections. INTRODUCTION the Kerman district, East-Central Iran; the fauna Late Ordovician and Early Silurian graptolites, they reported is that described in part from the from two areas in the northern part of the Zagros Katkoyeh Formation by Rickards et al. (1994), now belt (Figures 1, 2, 3), are described for the first time being fully described on the basis of collections from Iran.
    [Show full text]
  • Central Iran): Stratigraphy and Paleoenvironments
    Late Triassic and Early Cretaceous sedimentary sequences of the northern Isfahan Province 367 Boletín de la Sociedad GeolóGica Mexicana VoluMen 61, núM. 3, 2009, p. 367-374 D GEOL DA Ó E G I I C C O A S 1904 M 2004 . C EX . ICANA A C i e n A ñ o s Late Triassic and Early Cretaceous sedimentary sequences of the northern Isfahan Province (Central Iran): stratigraphy and paleoenvironments Maryam Mannani1,*, Mehdi Yazdi1 1 Department of Geology, University of Isfahan, Isfahan, Iran. * [email protected] Abstract This research gives a general outline of the Upper Triassic and Lower Cretaceous sequences cropping out north of Isfahan, Central Iran. Upper Triassic Nayband Formation subdivided into the Gelkan, Bidestan, Howz-e-Sheikh, Howz-e Khan and Qadir members. Two biostromal levels are documented in the Bidestan and Howz-e-Khan members. Due to a suitable condition in Late Triassic time including light, oxygen and nutrient, fauna such as: corals, sponges, hydrozoas, bivalves, gastropods, brachiopods, echinoderms and Dicroidium were flourished in water and flora on land. The first appearance of Heterastridium spp. in level of the Bidestan Member is apparently the first occurrence of this taxon in Central Iran. Qadir Member has several key beds, one key bed with land flora Cla- thropteris spp., and three key beds with bivalve Indopecten glabra, dating as Rhaetian Stage. An angular unconformity can be traced between Rhaetian sediments and red conglomerates and sandstones of Lower Cretaceous Sequences in Isfahan area which encompasses all Jurassic rocks. This gap can be related to Cimmerian tectonic phase.
    [Show full text]
  • The Earth's Lithosphere-Documentary
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/310021377 The Earth's Lithosphere-Documentary Presentation · November 2011 CITATIONS READS 0 1,973 1 author: A. Balasubramanian University of Mysore 348 PUBLICATIONS 315 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: Indian Social Sceince Congress-Trends in Earth Science Research View project Numerical Modelling for Prediction and Control of Saltwater Encroachment in the Coastal Aquifers of Tuticorin, Tamil Nadu View project All content following this page was uploaded by A. Balasubramanian on 13 November 2016. The user has requested enhancement of the downloaded file. THE EARTH’S LITHOSPHERE- Documentary By Prof. A. Balasubramanian University of Mysore 19-11-2011 Introduction Earth’s environmental segments include Atmosphere, Hydrosphere, lithosphere, and biosphere. Lithosphere is the basic solid sphere of the planet earth. It is the sphere of hard rock masses. The land we live in is on this lithosphere only. All other spheres are attached to this lithosphere due to earth’s gravity. Lithosphere is a massive and hard solid substratum holding the semisolid, liquid, biotic and gaseous molecules and masses surrounding it. All geomorphic processes happen on this sphere. It is the sphere where all natural resources are existing. It links the cyclic processes of atmosphere, hydrosphere, and biosphere. Lithosphere also acts as the basic route for all biogeochemical activities. For all geographic studies, a basic understanding of the lithosphere is needed. In this lesson, the following aspects are included: 1. The Earth’s Interior. 2.
    [Show full text]
  • Tectonostratigraphic Overview of the Zagros Suture Zone, Kurdistan Region, Northeast Iraq
    GeoArabia, 2012, v. 17, no. 4, p. 109-156 Gulf PetroLink, Bahrain Tectonostratigraphic overview of the Zagros Suture Zone, Kurdistan Region, Northeast Iraq Basim Al-Qayim, Azad Omer and Hemin Koyi ABSTRACT The northwestern segment of the Zagros Orogenic Belt of the Kurdistan Region of Iraq includes the Zagros Suture Zone which is consisting of allochthonous Tethyan Triassic–Eocene thrust sheets. The zone is bounded by the Zagros Main Reverse Fault in the northeast, and the Zagros Thrust Front in the southwest. Parts of this zone’s rocks are represented by stacks of thrust mega- sheets obducted over the autochthonous Cretaceous–Cenozoic sequence of the Arabian Plate margin. Each sheet represents a specific Tethyan tectono- stratigraphic facies, and includes (from older to younger): isolated Triassic carbonate platforms (Avroman Limestone), Jurassic carbonate imbricates (Chia Gara, Sargelu and other formations), radiolarites (Qulqula Group), sedimentary mélange (sedimentary-volcanic units of the Qulqula Group), ophiolites (Mawat and Penjwin ultramafics complexes), and Cenozoic fore-arc volcano- sedimentary sequences (Walash Group). Petrography, facies interpretation and lithostratigraphic correlation of these allochthons along four traverses across the Zagros Suture Zone of the examined area indicate that they evolved during the closure of the Neo-Tethys Ocean. Their stacking pattern and tectonic association resulted from two important events: the Late Cretaceous obduction processes, and the Late Miocene–Pliocene collision, uplift, folding and suturing between the Arabian Plate and the Sanandaj-Sirjan Block of Iran. Based on these field observations and by using the model of the Iranian Zagros evolution, a tectonic scenario is proposed to explain the history and evolution of the Zagros Suture Zone in this area.
    [Show full text]
  • Microfacies and Sedimentary Environments of Gurpi and Pabdeh Formations in Southwest of Iran
    American Journal of Applied Sciences 6 (7): 1295-1300, 2009 ISSN 1546-9239 © 2009 Science Publications Microfacies and Sedimentary Environments of Gurpi and Pabdeh Formations in Southwest of Iran Mohammad Bahrami Department of Geology, University of Payam-e-Noor, Shiraz, Iran Abstract: Problem statement: The Upper Cretaceous Gurpi and lower Tertiary Pabdeh formations as units of folded Zagros Zone were studied in three different regions (Tang-e-Abolhiat, Tang-e-Zanjiran and Maharloo) in Fars Province, Iran. Approach: Gurpi formation consisted of thin to medium sized layers of gray marl and marlstone interbedded with thin layers of argillaceous limestone and shale. The dominant microfacies in this formation biomicrite; Index species of Globotruncana give the age of the Formation from lower companion to upper Maastrichtian. Pabdeh formation consisted of bluish gray, thin to medium sized layers of shale and marl and interlayers of argillaceous limestones with purple shales and thin cherty beds at lower part, dark gray shales and marls with interlayers of argillaceous limestones in the middle andalternative layers of thinly bedded argillaceous limestone, shale and marl at the upper part. The dominant microfacies are biomicrite. Index species of Globorotalia and Hantkenina give the age of formation from upper Paleocene to Eocene. Results: The sedimentary environment of both formations is a bathymetrical carbonate floored basin (deep shelf or basin margin) which had deposited its facies in transgressive stage. The contact between the two formations is of disconformity type. In Tang-e-Abolhiat it lies at the base of purple shale. In this region and also in Tang-e-Zanjiran and Maharloo, in addition to recognition of Globorotalia velascoensis , which was attributed to lower part of the Pabdeh formation, a glauconitic- phosphatic bed separates the two formations.
    [Show full text]
  • Patricia Vickers-Rich1, Sara Soleimani2, Farnoosh Farjandi3, Mehdi Zand4, Ulf Linnemann5, Mandy Hofmann5, Thomas H
    New Discoveries in the Neoproterozoic of Iran Patricia Vickers-Rich1, Sara Soleimani2, Farnoosh Farjandi3, Mehdi Zand4, Ulf Linnemann5, Mandy Hofmann5, Thomas H. Rich1,6, Siobhan Wilson7 and Raymond Cas8 1. Faculty of Sci, Eng & Tech, Swinburne, Melbourne, Vic, Australia, [email protected]; School of EAE, Monash University, Melbourne, Vic, Australia, [email protected], 2. Paleontology Department, Geol Survey of Iran, Tehran, Iran, 3. Department of Geochemical Exploration, Geological Survey of Iran, Tehran, Iran, 4. Geology Department, Bafq Mining Company, Koushk Mine, Yazd, Iran, 5. Senckenberg Naturhistorische Sammlungen, Dresden, Museum fuer Mineralogie und Geologie, Sektion Geochronologie, Koenigsbruecker Landstrasse 159, D-01109, Dresden, Germany, 6. Museum Victoria, Exhibition Gardens, P. O. Box 666, Melbourne, Victoria, 3001 Australia, 7. University of Alberta, Earth & Atmospheric Science, Edmonton, Alberta, Canada, 8. School of EAE, Monash University, Melbourne, Vic, Australia Introduction During late 2015 new discoveries of Neoproterozoic metazoans were made in the Bafq Region of Central Iran by a joint Iranian-Australian expedition, hosted by the Iranian Geological Survey and the International Geological Program Project IGCP587. Previous to the newly discovered material supposed Vendian/Ediacaran metazoans including Permoria, Beltanella, and forms similar to Dickinsonia, Spriggina and Medusites (Stocklin, 1968), a supposed medusiod - Persimedusites chahgazensis (Hahn & Pflug 1980) along with Charnia (Glaessner, 1984) had been reported, but not well documented (Fedonkin et al., 2007). The new material both questions the identity of the previously described material and adds new taxa to the list of late Precambrian metazoans previously reported, increasing the biodiversity for this region. Pervious discoveries of Precambrian metazoans in Iran The first report of possible Neoproterozoic (Infracambrian) metazoan fossils from Iran was Stocklin (1968, 1972).
    [Show full text]
  • Tectonic Crossroads: Evolving Orogens of Eurasia-Africa-Arabia Conference Organizers
    Table of Contents Conference Organizers . 3 Preface . 5 Welcome from Chamber of Geological Engineers—Turkey . 6 Welcome from The Geological Society of America . 7 Welcome from Turkish Association of Petroleum Geologists . 8 Conference Schedule and Calendar of Events . 9 Technical Sessions Monday, 4 October . 13 Tuesday, 5 October . 16 Thursday, 7 October . 19 Friday, 8 October . 22 Abstracts . 25 Index of Authors . 88 2 Tectonic Crossroads: Evolving Orogens of Eurasia-Africa-Arabia Conference Organizers Co-Conveners Yildirim Dilek Miami University Department of Geology 116 Shideler Hall Oxford, OH 45056 U .S .A Erdin Bozkurt Middle East Technical University Department of Geological Engineering Ankara, 06531 Turkey Scientific Advisory Committee Erhan Altunel Osmangazi University, Turkey Erdin Bozkurt Middle East Technical University, TURKEY Sun-Lin Chung National Taiwan University, Taiwan Mark Cloos University of Texas at Austin, USA John Dewey University of California - Davis, USA; University College, U .K . Yildirim Dilek Miami University, USA W . Gary Ernst Stanford University; USA Harald Furnes University of Bergen, Norway Zvi Garfunkel Institute of Earth Sciences, The Hebrew University, Israel Robert Hall University of London, UK Akira Ishiwatari Center for Northeast Asian Studies, Tohoku University, JAPAN Laurent Jolivet Institut des Sciences de la Terre d’Orléans, Université d’Orléans-CNRS, France Kathleen Nicoll University of Utah, USA Yujiro Ogawa Tokyo Electric Power Services Co ., Ltd ., Japan Chang Whan Oh Chonbuk National
    [Show full text]
  • The Economic Geology of Iran Mineral Deposits and Natural Resources Springer Geology
    Springer Geology Mansour Ghorbani The Economic Geology of Iran Mineral Deposits and Natural Resources Springer Geology For further volumes: http://www.springer.com/series/10172 Mansour Ghorbani The Economic Geology of Iran Mineral Deposits and Natural Resources Mansour Ghorbani Faculty of Geoscience Shahid Beheshti University Tehran , Iran ISBN 978-94-007-5624-3 ISBN 978-94-007-5625-0 (eBook) DOI 10.1007/978-94-007-5625-0 Springer Dordrecht Heidelberg New York London Library of Congress Control Number: 2012951116 © Springer Science+Business Media Dordrecht 2013 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, speci fi cally the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on micro fi lms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. Exempted from this legal reservation are brief excerpts in connection with reviews or scholarly analysis or material supplied speci fi cally for the purpose of being entered and executed on a computer system, for exclusive use by the purchaser of the work. Duplication of this publication or parts thereof is permitted only under the provisions of the Copyright Law of the Publisher’s location, in its current version, and permission for use must always be obtained from Springer. Permissions for use may be obtained through RightsLink at the Copyright Clearance Center. Violations are liable to prosecution under the respective Copyright Law. The use of general descriptive names, registered names, trademarks, service marks, etc.
    [Show full text]
  • Estimation of Species Richness of Permian Foraminifera in Non-Parametric Methods and Investigation of Its Change Trend in Central Alborz, Western Tethys
    Open Journal of Geology, 2017, 7, 666-682 http://www.scirp.org/journal/ojg ISSN Online: 2161-7589 ISSN Print: 2161-7570 Estimation of Species Richness of Permian Foraminifera in Non-Parametric Methods and Investigation of Its Change Trend in Central Alborz, Western Tethys Mohammad Medadi1, Hossein Mosaddegh2, Seyed Mohsen Aleali3*, Mahmoud Reza Majidifard4 1Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran 2Department of Geology, Faculty of Earth Sciences, Kharazmi University of Tehran, Iran 3Department of Geology, Science and Research Branch, Islamic Azad University, Tehran, Iran 4Research Institute for Earth Sciences in Geological Survey of Iran, Tehran, Iran How to cite this paper: Medadi, M., Mo- Abstract saddegh, H., Aleali, S.M. and Majidifard, M.R. (2017) Estimation of Species Richness Species richness of foraminifera assemblages in the Permian succession, con- of Permian Foraminifera in Non-Parametric tains Dorud, Ruteh and Nessen Formations, in Central Alborz—North of Methods and Investigation of Its Change Iran, was estimated and studied based on lithostratigraphy and microbiostra- Trend in Central Alborz, Western Tethys. Open Journal of Geology, 7, 666-682. tigraphy of Permian. We used four non-parametric estimators to investigate https://doi.org/10.4236/ojg.2017.75045 the species richness: Chao 2, Jackknife 1, Jackknife 2 and bootstrap. These methods estimates the species richness based on the presence/absence data of Received: December 26, 2016 each taxon identified in the samples. We use the submenu of quadrat richness Accepted: May 21, 2017 Published: May 24, 2017 in “Past” [1] software to estimate richness in regional chronostratigraphic stages.The results show that the estimated diversity of foraminiferal assem- Copyright © 2017 by authors and blages with the exception of late Yakhtashian, increased constantly from Asse- Scientific Research Publishing Inc.
    [Show full text]
  • Fasciculate Kleopatrinid Corals from the Bashkirian (Late Carboniferous) of Sardar Formation (Ozbak-Kuh Mountains, East-Central Iran)
    Rev. bras. paleontol. 19(2):151-166, Maio/Agosto 2016 © 2016 by the Sociedade Brasileira de Paleontologia doi: 10.4072/rbp.2016.2.01 FASCICULATE KLEOPATRINID CORALS FROM THE BASHKIRIAN (LATE CARBONIFEROUS) OF SARDAR FORMATION (OZBAK-KUH MOUNTAINS, EAST-CENTRAL IRAN) MAHDI BADPA Department of Geology, Faculty of Science, Ferdowsi University of Mashhad, Mashhad, Iran. [email protected] EDOUARD POTY Paléontologie animale et humaine, Département de Géologie, Université de Liège, Bât.B18, Allée du 6 Août, Sart Tilman, 4000-Liège, Belgium. [email protected] ALIREZA ASHOURI Department of Geology, Faculty of Science, Ferdowsi University of Mashhad, Mashhad, Iran. [email protected] KAVEH KHAKSAR Department of Water & Soil, Imam Khomeini High Education Center, Institute of Scientific Applied Higher Education of Jihad-e-Agriculture, Karaj, Iran. [email protected] ABSTRACT – In the East-Central Iran, the Sardar Formation (upper Visean–Moscovian) consists of shallow-water limestone with intercalations of shale containing rugose corals, tabulate corals and brachiopods. Ten sections were sampled in the Ozbak-kuh Mountains, from north to south. Among the rugose corals, an assemblage of fasciculate Kleopatrinidae has been collected. The latter contains the species: Paraheritschioides antoni antoni, P. antoni minor, P. gracilis and two new species for the genera Fomichevella and Heintzella. Heintzella is described from Iran for the first time. However, its age, as determined by conodonts and foraminifers, is early to middle Bashkirian (early late Carboniferous). The most similar, time-equivalent faunal associations are that of the Ellesmere Island, Sverdrup Basin in Arctic Canada, Alexander terrane and Brooks Range in southeastern Alaska and eastern Klamath terrane in northern California, where similar tropical warm water conditions have been identified during the Bashkirian in the northern hemisphere.
    [Show full text]