The Permian-Triassic Transition in the Oman Mountains
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Bulletin Contributions to the Knowledge of Richthofenia Inthe
Bulletin of the University of Texas 1916: No. 55 October 1, 1916 Bureau of Economic Geology and Technology J. A.Udden, Director Contributions to the Knowledge of Richthofenia in the Permian of West Texas By EmilBose Published by the University six- times a month and entered as second-class mail matter at the postoffice at AUSTIN, TEXAS PUBLICATIONS OF THE BUREAU OF ECONOMIC GEOLOGY AND TECHNOLOGY The Mineral Resources of Texas. Win. B. Phillips. Issued by the State Department of Agriculture as its Bulletin No. 14, July-August, 1910. (Out of print.) The Composition of Texas Coals and Lignites and the Use of Producer Gas in Texas. Wm. B. Phillips, S. H. Worrell, and Drury McN.- Phillips. University of Texas Bulletin No. 189, July, 1911. (Out of print.) A Reconnaissance Report on the Geology of the Oil and Gas Fields of Wichita and Clay Counties. J. A. Udden, assisted by Drury McN. Phillips. University of Texas Bulletin No. 246, September, 1912. Price, 50 cents. The Fuels Used in Texas. Wm. B. Phillips and S; H. Worrell. Univer- sity of Texas Bulletin No. 307, December 22, 1913. Price, 40 cents. The Deep Boring at Spur. J. A. Udden. University of Texas Bulletin No. 363, October 5, 1914. (Out of print.) The Mineral Resources of Texas. Wm. B. Phillips. University of Texas Bulletin No. 365, October 15, 1914. Price, 50 cents. Potash in the Texas Permian. J. A. Udden. University of Texas Bulletin No. 17, March 20, 1915. Price, 10 cents. Geology and Underground Waters of the Northern Llano Estacado, Charles Laurence Baker. -
Oases of Oman Livelihood Systems at the Crossroads
oases of oman livelihood systems at the crossroads Second EXPANDED edition AL ROYA PRESS & PUBLISHING HOUSE MUSCAT sponsored by University of agriculture, faisalabad, Pakistan The front cover of this volume shows the main terrace system of the 3,000 year old oasis of Biladsayt in the northern Al Hajar mountain range and the back page variation in irrigated wheat planting as a farmer strategy to cope with year-specific water availability during 2003, 2006 and 2007 in the agro-pastoral oasis of Maqta in the eastern Jabal Bani Jabir range of Oman. Al Roya Press & Publishing House P. O. Box 343, Postal Code 118, Al Harthy Complex, Muscat, Sultanate of Oman Tel: (968) 24 47 98 81/882/883/884/885/886/887/888, Fax: (968) 24 47 98 89 E-mail: [email protected] www.alroya.net © Compilation: Andreas Buerkert and Eva Schlecht © Individual texts: Named authors Publisher: Hatim Al Taie Editors: Andreas Buerkert and Eva Schlecht In-house Editor: Helen Kirkbride Dr. Muhammad Jalal Arif, Principal Officer Public Relations & Publications (PRP) Dept. University of Agriculture, Faisalabad, Pakistan Design & Production: Dhian Chand Mumtaz Ali Officer Incharge, University Press University of Agriculture, Faisalabad, Pakistan Printed by: University Press University of Agriculture Faisalabad, Pakistan Second Published: November 2010 ISBN: 978-969-8237-51-6 Note: Data and literature complementing the information collected in this book can be accessed on the internet at: http://www.oases-of-oman.org contents Foreword 5 Authors 6 Introduction 7 Chapter 1 8 -
Welcome to Anantara Al Jabal Al Akhdar Resort a Guide to Etiquette, Climate and Transportation
EXPERIENCE NEW HEIGHTS OF LUXURY WITH AUTHENTIC OMANI HOSPITALITY WELCOME TO ANANTARA AL JABAL AL AKHDAR RESORT A GUIDE TO ETIQUETTE, CLIMATE AND TRANSPORTATION ETIQUETTE As a general courtesy with respect to local customs, it is highly recommended to dress modestly whilst out and about in Oman. We suggest for guests to cover their shoulders and legs (from the knee up), and to avoid form fitting clothing. CLIMATE Al Jabal Al Akhdar is known for its Mediterranean climate. Temperatures drop during winter to below zero degrees Celsius with snow falling at times, and rise in the summer to 28 degrees Celsius. TRANSPORTATION Kindly be informed that you need a 4x4 vehicle to pass by the check point for Al Jabal Al Akhdar, along with your driving license and car registration papers. If you are not driving a 4x4 vehicle, you may park near the check point and request for us to arrange a luxury 4x4 transfer to the resort. Please contact us at tel +968 25218000 for more information. TOP 10 FUN THINGS TO DO IN AL JABAL AL AKHDAR 1. Kids Camping 2. Rock Climbing 3. Wadi of Waterfalls Hike 4. Via Ferrata Mountain Climbing 5. Stargazing 6. Cycling Tours 7. Three Village Adventure Treks 8. Sundown Journey Tour 9. Morning Yoga 10. Archery Lessons DIRECTIONS TO ANANTARA AL JABAL AL AKHDAR RESORT Seeb MUSCAT Muscat International Airport 15 15 Nizwa / Salalah Exit 15 Jabal Akhdar Hotel Samail 15 15 Jabal Akhdar Hotel FROM MUSCAT 172 KM / 2HR 15MIN Use the Northwest expressway out of Muscat heading towards Seeb, and turn off at the Nizwa/Salalah exit and continue following signs towards Izki / Nizwa. -
Al Alama Centre
ALAL AMANAALAMAALAMA CENTRECENTRECENTRE MUSCAT,MUSCAT, SULTANATESULTANATE OFOF OMANOMAN HH AA NN DD BB OO OO KK 0 OUR HISTORY – A UNIQUE LEGACY The name “Al Amana” is Arabic for “bearing trust,” which captures the spirit and legacy of over 115 years of service in Oman. The Centre is the child of the Gulf-wide mission of the Reformed Church in America that began in Oman in 1893. The mission‟s first efforts were in educational work by establishing a school in 1896 that eventually became a coeducational student body of 160 students. The school was closed in 1987 after ninety years of service to the community. The mission was active in many other endeavors, which included beginning a general hospital (the first in Oman), a maternity hospital, a unit for contagious diseases, and a bookshop. With the growth of these initiatives, by the 1950‟s the mission was the largest employer in the private sector in Oman. In the 1970‟s the hospitals were incorporated in the Ministry of Health, and the mission staff worked for the government to assist in the development of its healthcare infrastructure. The mission also established centers for Christian worship in Muscat and Muttrah. It is out of these centers that the contemporary church presence for the expatriate community Oman has grown, now occupying four campuses donated by His Majesty Sultan Qaboos bin Said. After Oman discovered oil, having a newfound wealth with which to modernize, the mission's activities were either concluded or grew into independent initiatives. However, the desire to serve the people of Oman continued. -
Geochemical Characterization, Petrogenetic Modelling And
Geochemical characterization, petrogenetic modelling and engineering behaviour of granitic rocks and basic dykes from the northern Indian plate in north-western Pakistan Muhammad Sajid Submitted to the University of Exeter as a thesis for the degree of Doctor of Philosophy in Geology in September 2016 This thesis is available for Library use on the understanding that it is copyright material and that no quotation from the thesis may be published without proper acknowledgement. I certify that all material in this thesis which is not my own work has been identified and that no material has previously been submitted and approved for the award of a degree by this or any other University. Signature: ………………………………………………………….. September 2016 1 Abstract The pre-Himalayan magmatic events along the northern margin of Indian plate in north-western Pakistan have been investigated and correlated with analogous magmatism in other Himalayan and northern Gondwana regions. The samples from Utla and Mansehra regions of NW Pakistan are dominantly megacrystic two mica granites, strongly peraluminous (A/CNK > 1.1) and intruded by aplite dykes and quartz-rich veins. The high precision zircon U-Pb ages (471-479 Ma) show their emplacement in early Paleozoic. These granites are enriched in light rare- earth elements (LREEs) and show similar chondrite normalized REE patterns with negative Eu anomalies (Eu/Eu* = 0.07–0.73). The geochemical signature and REE based modelling indicate that the granites are derived mainly from the partial melting of pelitic source followed by the evolution of melt via fractional crystallization resulting in the formation of aplites. Tourmaline occurrences in distinct modes show post-magmatic alteration of these granites triggered by hydrothermal fluids from different sources. -
Gondwana Large Igneous Provinces (Lips): Distribution, Diversity and Significance
Downloaded from http://sp.lyellcollection.org/ by guest on September 25, 2021 Gondwana Large Igneous Provinces (LIPs): distribution, diversity and significance SARAJIT SENSARMA1*, BRYAN C. STOREY2 & VIVEK P. MALVIYA3 1Centre of Advanced Study in Geology, University of Lucknow, Lucknow, Uttar Pradesh 226007, India 2Gateway Antarctica, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand 324E Mayur Residency Extension, Faridi Nagar, Lucknow, Uttar Pradesh 226016, India *Correspondence: [email protected] Abstract: Gondwana, comprising >64% of the present-day continental mass, is home to 33% of Large Igneous Provinces (LIPs) and is key to unravelling the lithosphere–atmosphere system and related tectonics that mediated global climate shifts and sediment production conducive for life on Earth. Increased recognition of bimodal LIPs in Gondwana with significant, sometimes subequal, proportions of synchronous silicic volcanic rocks, mostly rhyolites to high silica rhyolites (±associ- ated granitoids) to mafic volcanic rocks is a major frontier, not considered in mantle plume or plate process hypotheses. On a δ18O v. initial 87Sr/86Sr plot for silicic rocks in Gondwana LIPs there is a remarkable spread between continental crust and mantle values, signifying variable contributions of crust and mantle in their origins. Caldera-forming silicic LIP events were as large as their mafic counterparts, and erupted for a longer duration (>20 myr). Several Gondwana LIPs erupted near the active continental margins, in addition to within-continents; rifting, however, continued even after LIP emplacements in several cases or was aborted and did not open into ocean by coeval com- pression. Gondwana LIPs had devastating consequences in global climate shifts and are major global sediment sources influencing upper continental crust compositions. -
Permophiles Issue
Contents Notes from the SPS Secretary ...........................................................................................................................1 Shen Shuzhong Notes from the SPS Chair ..................................................................................................................................2 Charles M. Henderson Meeting Report: Report on the Continental Siena Meeting, Italy, September 2006.....................................3 G. Cassinis, A. Lazzarotto, P. Pittau Working Group Report: Short report on 2005-2006 activities of the non-marine – marine correlation work- ing group of SPS ..................................................................................................................................................5 J.W. Schneider Report of SPS Working Group on “Using Permian transitional biotas as gateways for global correlation”7 Guang R. Shi International Permian Time Scale ...................................................................................................................10 Voting Members of the SPS ............................................................................................................................. 11 Submission guideline for Issue 49 ....................................................................................................................12 Reports: Ostracods (Crustacea) from the Permian-Triassic boundary interval of South China (Huaying Mountains, eastern Sichuan Province): paleo-oxygenation significance .......................................................12 -
Website Reference List.Xlsx
TLS Reference List 16-07-19 Type Project Name Client Project Type Region Completion Year 33kV Project Construction Of New Saham -2, 2x20MVA Primary Substation Majan Electricity Company Substation Al Batinah North Governorate 2016 33kV Project Construction of New Juffrh, 2 x20MVA primary Substation Majan Electricity Company Substation Al Batinah North Governorate 2016 33kV Project Construction of New Mukhailif - 2 , 2x20MVA Primary Substation Majan Electricity Company Substation Al Batinah North Governorate 2016 33kV Project Al Aman Camp at Bait Al Barka Primary 33/11kv Electrical Substation. Royal Court Affairs Substation Al Batinah South Governorate 2012 33kV Project DPC_Construction Of 1x6MVA, 33/11KV Indoor Primary Substation Designate as Al Saan Dhofar Power Company Substation Dhofar Governorate 2016 33kV Project DPC_Construction Of 1x6MVA, 33/11KV Indoor Primary Substation Designate as Teetam Dhofar Power Company Substation Dhofar Governorate 2016 33kV Project DPC_Construction Of 1x6MVA, 33/11KV Indoor Primary Substation Designate as Hakbeet Dhofar Power Company Substation Dhofar Governorate 2016 33kV Project Upgrading Of Al Jiza, Al Quwaiah, Al Ayoon & Al Falaj Primary Sub stations (33/11 KV) at Mudhaibi Mazoon Electricity Company Substation Ash Sharqiyah North Governorate 2015 Construction of 33KV Feeder from Seih Al Khairat Power station to the Proposed 2x10 MVA , 33/11KV Primary S/S at Hanfeet to feed Power Supply to Hanfeet Power Supply to Hanfeet farms - Wilayat 33kV Project Thumrait Rural Areas Electricity Company (Tanweer) -
Large Igneous Provinces and Mass Extinctions: an Update
Downloaded from specialpapers.gsapubs.org on April 29, 2015 OLD G The Geological Society of America Special Paper 505 2014 OPEN ACCESS Large igneous provinces and mass extinctions: An update David P.G. Bond* Department of Geography, Environment and Earth Science, University of Hull, Hull HU6 7RX, UK, and Norwegian Polar Institute, Fram Centre, 9296 Tromsø, Norway Paul B. Wignall School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK ABSTRACT The temporal link between mass extinctions and large igneous provinces is well known. Here, we examine this link by focusing on the potential climatic effects of large igneous province eruptions during several extinction crises that show the best correlation with mass volcanism: the Frasnian-Famennian (Late Devonian), Capi- tanian (Middle Permian), end-Permian, end-Triassic, and Toarcian (Early Jurassic) extinctions. It is clear that there is no direct correlation between total volume of lava and extinction magnitude because there is always suffi cient recovery time between individual eruptions to negate any cumulative effect of successive fl ood basalt erup- tions. Instead, the environmental and climatic damage must be attributed to single- pulse gas effusions. It is notable that the best-constrained examples of death-by- volcanism record the main extinction pulse at the onset of (often explosive) volcanism (e.g., the Capitanian, end-Permian, and end-Triassic examples), suggesting that the rapid injection of vast quantities of volcanic gas (CO2 and SO2) is the trigger for a truly major biotic catastrophe. Warming and marine anoxia feature in many extinc- tion scenarios, indicating that the ability of a large igneous province to induce these proximal killers (from CO2 emissions and thermogenic greenhouse gases) is the single most important factor governing its lethality. -
The Anglo-Omani Society Review 2016
New Generation Group Edition Across the Rub al Khali …IN THE STEPS OF BERTRAM THOMAS AND BIN KALUT William&Son_2016_Layout 1 19/09/2016 16:42 Page 1 003-005 - Contents&Officers_Layout 1 19/09/2016 11:50 Page 3 JOURNAL NO. 80 COVER PHOTO: In the Footsteps of Bertram Thomas Photo Credit: John Smith CONTENTS 6 CHAIRMAN’S OVERVIEW 51 OMAN IN THE YEARS OF THE FIRST WORLD WAR 8 THE 40th ANNIVERSARY OF THE ANGLO-OMANI SOCIETY 53 NEW GENERATION GROUP INTRODUCTION A HISTORY OF NGG EVENTS NGG IN OMAN NGG DELEGATIONS 2013-15 NGG DELEGATION 2016 SOCIAL MEDIA OMANI STUDENTS UK INTERNSHIP PROGRAMME NGG’S PARTNER ORGANISATIONS MOHAMMED HASSAN PHOTOGRAPHY 14 IN THE FOOTSTEPS OF BERTRAM THOMAS 20 THE ROYAL CAVALRY OF OMAN 88 EDUCATIONAL OPPORTUNITIES 93 THE ‘ABC’ OF OMAN INSECTS 96 ANGLO-OMANI LUNCHEON 22 UNDER THE MICROSCOPE: A CLOSER LOOK AT OMANI SILVER 98 THE SOCIETY’S GRANT SCHEME 26 THE ESMERALDA SHIPWRECK OFF 100 ARABIC LANGUAGE SCHEME AL HALLANIYAH ISLAND 105 AOS LECTURE PROGRAMME 29 MUSCAT “THE ANCHORAGE” 106 THE ANGLO-OMANI SOCIETY 34 OMAN THROUGH THE EYES OF GAP YEAR SCHEME SUE O’CONNELL 108 SUPPORT FOR YOUNG OMANI SCHOLARS 36 BAT OASIS HERITAGE PROJECT 110 LETTER TO THE EDITOR 40 OMAN THROUGH THE EYES OF PETER BRISLEY 112 BOOK REVIEWS 42 THE BRITISH EMBASSY: RECOLLECTIONS OF THE FIRST AMBASSADRESS 114 MEET THE SOCIETY STAFF 46 ROYAL GUESTS AT A RECEPTION 115 WHERE WAS THIS PHOTOGRAPH TAKEN? 3 003-005 - Contents&Officers_Layout 1 19/09/2016 11:50 Page 4 THE ANGLO-OMANI SOCIETY Society Address 34, Sackville Street, London W1S 3ED +44 (0)20 7851 7439 Patron www.angloomanisociety.com HM Sultan Qaboos bin Said Advertising Christine Heslop 18 Queen’s Road, Salisbury, Wilts. -
Permian (Artinskian to Wuchapingian) Conodont Biostratigraphy in the Tieqiao Section, Laibin Area, South China
Permian (Artinskian to Wuchapingian) conodont biostratigraphy in the Tieqiao section, Laibin area, South China Y.D. Suna, b*, X.T. Liuc, J.X. Yana, B. Lid, B. Chene, D.P.G. Bondf, M.M. Joachimskib, P.B. Wignallg, X.L. Laia a State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, 430074, China b GeoZentrum Nordbayern, Universität Erlangen-Nürnberg, Schlossgarten 5, 91054 Erlangen, Germany c Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China d Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Ministry of Land and Resources, Guangzhou, 510075, China e State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, 39 East Beijing Road, Nanjing, 210008, R.P. China f School of Environmental Sciences, University of Hull, Hull HU6 7RX, UK g School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK *Corresponding authors Email: [email protected] (Y.D. Sun) © 2017, Elsevier. Licensed under the Creative Commons Attribution- NonCommercial-NoDerivatives 4.0 International http://creativecommons.org/ licenses/by-nc-nd/4.0/ 1 Abstract Permian strata from the Tieqiao section (Jiangnan Basin, South China) contain several distinctive conodont assemblages. Early Permian (Cisuralian) assemblages are dominated by the genera Sweetognathus, Pseudosweetognathus and Hindeodus with rare Neostreptognathodus and Gullodus. Gondolellids are absent until the end of the Kungurian stage—in contrast to many parts of the world where gondolellids and Neostreptognathodus are the dominant Kungurian conodonts. A conodont changeover is seen at Tieqiao and coincided with a rise of sea level in the late Kungurian to the early Roadian: the previously dominant sweetognathids were replaced by mesogondolellids. -
Biostratigraphy of the Phosphoria, Park City, and Shedhorn Formations
Biostratigraphy of the Phosphoria, Park City, and Shedhorn Formations GEOLOGICAL SURVEY PROFESSIONAL PAPER 313-D Work done partly on behalf of the U.S. Atomic Energy Commission Biostratigraphy of the Phosphoria, Park City, and Shedhorn Formations By ELLIS L. YOCHELSON With a Section on Fish By DIANNE H. VAN SICKLE GEOLOGY OF PERMIAN ROCKS IN THE WESTERN PHOSPHATE FIELD GEOLOGICAL SURVEY PROFESSIONAL PAPER 313-D Work done partly on behalf of the U.S. Atomic Energy Commission Distribution of megafossils in more than collections, mainly from measured sections^ and their paleoecological interpretation UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 60 cents (paper cover) CONTENTS Page Page Abstract., ________________________________________ 571 Age of the Phosphoria and correlative formations Con. Introduction.______________________________________ 572 Shedhorn Sandstone.__________-____----------__ 626 Stratigraphic setting.___________________________ 573 Summary of age relationships,___________________ 627 Previous work..________________________________ 573 Geographic distribution of collections-________-___---- 630 Acknowledgments ______________________________ 574 Grandeur Member of Park City Formation-------- 630 Pr ocedures_ ________________________________________ 574 Idaho-__________________________________