Sedimentation and Tectonics of Lower Cenozoic Sequences From
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Early Cretaceous Alkaline/Ultra-Alkaline
300 Article 300 by Rajesh K. Srivastava Early Cretaceous alkaline/ultra-alkaline silicate and carbonatite magmatism in the Indian Shield – a review: implications for a possible remnant of the Greater Kerguelen Large Igneous Province Department of Geology, Centre of Advanced Study, Institute of Science, Banaras Hindu University, Varanasi 221005, India; Email: [email protected] (Received : 12/01/2019; Revised accepted : 24/07/2019) https://doi.org/10.18814/epiiugs/2020/020017 ABSTRACT alkaline/ultra-alkaline silicate rocks is directly related to the nature The early Cretaceous (ca. 118-100 Ma) alkaline/ultra- and source of melts and their crystallization history. The origin of carbonated silicate melts through liquid-immiscibility or fractional alkaline silicate and carbonatite magmatism, exclusively crystallization suggest genetic connection between carbonate and recorded in the Chhotanagpur Gneissic Complex and silicate derivatives, whereas direct genetic connection between these the Shillong Plateau-Mikir Hills in the eastern/north- two rocks is uncertain if derived directly from low-degree partial eastern regions of the Indian Shield, have been reviewed melts of carbonated mantle peridotite at deeper level (cf. Bell et al., to understand their genetic aspects. These are thought 1998; Gittins and Harmer, 2003; Srivastava et al., 2005; Mitchell, 2005; Melluso et al., 2010; Beccaluva et al., 2017). Furthermore, the to be associated to the Kerguelen hot spot, active in this spatial and temporal connections between carbonatites and Large region during ca. 118-100 Ma. The existing geochemical, Igneous Provinces (LIPs), and ultimately to plume tectonics, are also geochronological and isotopic data do not support any well established (e.g. Simonetti et al., 1998; Bell and Tilton, 2001; definite emplacement order for these diverse groups of Campbell, 2005; Ernst, 2014; Bryan and Ernst, 2008; Ernst and Bell, magmatic suites. -
Assam: State Geology and Mineral Maps
GSI Misc. Pub. 30 Pt. 4 Vol. 2(i) PGSI. 307 700-2009 (DSK-II) GEOLOGY AND MINERAL RESOURCES OF ASSAM GEOLOGICAL SURVEY OF INDIA Miscelleaneous Publication No. 30 Part IV Vol 2(i) Assam 150 YEARS in the service of the nation Published by the order of the Government of India 2009 GSI Misc. Pub. 30 Pt. 4 Vol. 2(i) Copy right © India, Geological Survey, 2009 First Edition : 2009 Second Reprint s: March, 2011 Manuscript processed for printing by: G. K. KESARI Geologist (Sr) under the guidance of : G. DAS GUPTA B. V. R. REDDY DR. H.S.M. PRAKASH Director Director AND Director Publication Division Publication Division Publication Division Overall supervision by: B.K. Mohanty Sudipta Lahiri U.K.Behara Ex-Dy. Director General Dy. Director General AND Director In-Charge Geological Survey of India NORTH EASTERN REGION Shillong- 793 003 Printed at ESSAR OFFSET Janapath Lane, G.S. Road, Ulubari, Guwahati-781007, Mobile : +91-9435106080 Price: Inland : Rs. 84/- Foreign : £ 3.31 or $ 4.61 GSI Misc. Pub. 30 Pt. 4 Vol. 2(i) FOREWORD The Miscellaneous Publication 30 Series of the Geological Survey of India brings out concise information on the geology and mineral resources of the states of India. The present volume Part IV, Vol. 2(i) of the series, pertaining to the state of Assam, is a revised and updated version of the first edition published in 1974. During the span of three decades since the first edition was published, enormous knowledge has been added in the sphere of geology of the area, hence warranting publication of a revised edition. -
Regional Divisions of India a Cartographic Analysis, Vol-XIV
CENSUS OF INDIA REGIONAL DIVISIONS OF INDIA -A CARTOGRAPHIC ANALYSIS OCCASIONAL PAPERS SERIES-1 VOLUME-XIV MEGHALAYA Planning & Supervision B.K. ROY, M.A., Ph. D. Deputy Registrar General (Map) General Direction & Editing VIJAY S. VERMA of the Indian Administrative Service Registrar General & Census Commissioner, India 2 - A, Mansingh Road, New Delhi Maps included in this volume are based upon Survey of India map with the permission of the Surveyor General of India. The boundary of Meghalaya shown on the map of India is as interpreted from North-eastern areas (Reorganisa tion) Act, 1971, but has yet to be verified (applicable to India map only). The territorial waters of India extend into the sea to a distance of twelve nautical miles measured from the appropriate base line (applicable to India map only). The Indo-Bangladesh boundary shown on this map is the one existing prior to the conclusion of the agreement of May 16, 1974 between India and Bangladesh. © Government of India Copyright 1988. ~~ ~ ~~-~ HOME MINISTER INDIA NEW DELHI-110001 Oct. 26, 1988 FOREWORD Experience has taught us that planning has to be related the situation in the field in 0 rder to better respond to .Iocal aspirations and for better utilization of local resources. A lot of planning has, of necessity, t9 be for larger areas, encompassing an agglomeration of administrative units. Even such macro planning has, in order to be realistic, to be cognisant of the realities at the micro level. Correspondingly, such plans for bigger areas and involving larger outlays have also to be admini stered from a suitably high threshold of administrative authority and by a wide network of administra tive hierarchy. -
Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1955 Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys. S. Ali ibne hamid Rizvi Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Rizvi, S. Ali ibne hamid, "Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys." (1955). LSU Historical Dissertations and Theses. 109. https://digitalcommons.lsu.edu/gradschool_disstheses/109 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. COMPARATIVE PHYSIOGRAPHY OF THE LOWER GANGES AND LOWER MISSISSIPPI VALLEYS A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography ^ by 9. Ali IJt**Hr Rizvi B*. A., Muslim University, l9Mf M. A*, Muslim University, 191*6 M. A., Muslim University, 191*6 May, 1955 EXAMINATION AND THESIS REPORT Candidate: ^ A li X. H. R iz v i Major Field: G eography Title of Thesis: Comparison Between Lower Mississippi and Lower Ganges* Brahmaputra Valleys Approved: Major Prj for And Chairman Dean of Gri ualc School EXAMINING COMMITTEE: 2m ----------- - m t o R ^ / q Date of Examination: ACKNOWLEDGMENT The author wishes to tender his sincere gratitude to Dr. Richard J. Russell for his direction and supervision of the work at every stage; to Dr. -
Physical Features, Climate and Drainage of India Hand Outs
INDIA PHYSIOGRAPHIC DIVISIONS India is the seventh largest and second most populous country in the world. Its area is 2.4% of the total world area but about 16% of the entire human races reside in its fold. In population, only the mainland China exceeds that of India. India, Pakistan, Bangladesh, Nepal and Bhutan form the well-defined realm of south Asia often referred to as the Indian sub-continent. Lying entirely in the northern hemisphere (tropical zone), the Indian mainland extends between the latitude -8°4' N to 37°6'N and longitude -68°7' E to 97°25'E. The southernmost point in the Indian territory, the Indira Point, is situated at 6°30' north in the Andaman and Nicobar islands. The tropic of cancer passes through the centre of India. India covers an area of 3.28 million sq km and measures about 3,214 km from north to south and about 2,933 km east to west. The total length of the mainland coastland is nearly 6,400 km and land frontier about 15,200 km. The boundary line between India and China is called the McMahon line. To the north-west, India, shares a boundary mainly with Pakistan and to the east with Myanmar and Bangladesh. The Indian Ocean lies in the south. In the south, on the eastern side, the Gulf of Mannar and the Palk Strait separate India from Sri Lanka. The Andaman and Nicobar Islands in the Bay of Bengal and the Lakshadweep islands in the Arabian Sea are parts of the Indian Territory India's relief is marked by a great variety: India can be divided into five major physiographic units: 1. -
Geology, Structure and Tectonics of Shillong Plateau
© 2018 JETIR August 2018, Volume 5, Issue 8 www.jetir.org (ISSN-2349-5162) GEOLOGY, STRUCTURE AND TECTONICS OF SHILLONG PLATEAU Laishram Sherjit Singh and Kh Mohon Singh Department of Environmental Studies, NEHU Shillong Department of Geology, Imphal College, Imphal Abstract-Shillong Plateau is located in the north eastern part of India. It exposes almost all kinds of rocks from Precambrian to recent. It is tectonically and seismically very active. The 1897 Great Shillong earthquake occurred at western edge of the Shillong Plateau and it uplifted the northern part of it about 10m. It captures the attention of many geoscientists. Geoscientists have been investigating the Shillong Plateau using many tools and techniques for better understanding of geology, structure and tectonics as major earthquakes are related to tectonic movements. Interestingly, it gives different results about the mechanism of upliftment of Shillong Plateau and how it detaches from Indian Shield and moves towards east to its present position. In this paper, we are presenting a brief review about geology, tectonics and structural features of Shillong Plateau. A detailed stratigraphic succession is compiled based on different sources. Keywords: Shillong Plateau, Indian Shield, Precambrian, Tectonics, Upliftment Introduction Shillong Plateau which is also known as Meghalaya Plateau is a part of the Indian Shield (Evans 1964). This plateau is bounded by the Dauki fault to the south, Kopili fault to the east, Brahmaputra fault to the north and Dhubri fault to the west. It covers an area of about 25,000 km2 (Chen and Molanar, 1990) and criss-crossed by many faults. It is separated from Indo- Myanmar Mobile belt by NE-SW trending belt of Schuppen and from Eastern Himalayas by Brahmaputra River. -
Geochemistry and Petrogenesis of Early Cretaceous Sub-Alkaline Mafic
Geochemistry and petrogenesis of early Cretaceous sub-alkaline mafic dykes from Swangkre-Rongmil, East Garo Hills, Shillong plateau, northeast India Rajesh K Srivastava∗ and Anup K Sinha Igneous Petrology Laboratory, Department of Geology, Banaras Hindu University, Varanasi 221 005, India. ∗e-mail: [email protected] Numerous early Cretaceous mafic and alkaline dykes, mostly trending in N-S direction, are emplaced in the Archaean gneissic complex of the Shillong plateau, northeastern India. These dykes are spatially associated with the N-S trending deep-seated Nongchram fault and well exposed around the Swangkre-Rongmil region. The petrological and geochemical characteristics of mafic dykes from this area are presented. These mafic dykes show very sharp contact with the host rocks and do not show any signature of assimilation with them. Petrographically these mafic dykes vary from fine-grained basalt (samples from the dyke margin) to medium-grained dolerite (samples from the middle of the dyke) having very similar chemical compositions, which may be classified as basaltic-andesite/andesite. The geochemical characteristics of these mafic dykes sug- gest that these are genetically related to each other and probably derived from the same parental magma. Although, the high-field strength element (+rare-earth elements) compositions disallow the possibility of any crustal involvement in the genesis of these rocks, but Nb/La, La/Ta, and Ba/Ta ratios, and similarities of geochemical characteristics of present samples with the Elan Bank basalts and Rajmahal (Group II) mafic dyke samples, suggest minor contamination by assimilation with a small amount of upper crustal material. Chemistry, particularly REE, hints at an alkaline basaltic nature of melt. -
Asian Journal of Multidisciplinary Studies (AJMS)
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Asian Journal of Multidisciplinary Studies (AJMS) ISSN: 2321-8819 (Online) Asian Journal of 2348-7186 (Print) Impact Factor: 0.92 Multidisciplinary Studies Volume 3, Issue 2, Feb. 2015 Geochemistry of Mesoproterozoic metadolerite dykes and sills of Shillong basin, Meghalaya, NE India K.P. Sarma*, J.J. Laskar, Niva Rani Devi, Nandita Mazumdar, J. Mallikharjuna Rao and M. Venkateshwarlu 1Professor – (Rtd.), Department of Geological Sciences, Gauhati University, Guwahati – 781014, India. 2Assistant Professor, Department of Geological Sciences, Gauhati University, Guwahati – 781014, India. 3Assistant Professor, Arya Vidyapeeth College, Guwahati 781016, India. 4Research Scholar, Department of Geological Sciences, Gauhati University, Guwahati – 781014, India. 5Retired Scientist, National Geophysical Research Institute, Uppal Road, Hyderabad 500 606, India 6Scientist E, National Geophysical Research Institute, Uppal Road, Hyderabad 500 606, India. Abstract The Shillong Basin is the only Proterozoic (Purana) basin of NE India and is an intracratonic sag basin in nature. The basin is dominantly exposed in Meghalaya and partly in Karbi Anglong district of Assam and confined in the central and eastern parts of the Shillong plateau. This Proterozoic basin was developed during early Mesoproterozoic time. The metasedimentary rock associations of this basin are classified under Lower Metapelitic and Upper Quartzitic Formations closely associated with mafic magmatism in the form of mafic sills and dykes (metadolerite, locally named as Khasi greenstone). They are metamorphosed under greenschist – amphibolite transitional facies. The present study aims at generating geochemical characteristics of the metadolerites of the basin. Mafic dykes and sills of the basement of the Shillong plateau is of Cretaceous age and excluded from the present study. -
D:\Pinsa 2020\March-Iugs\Map\Ma
Volume 86 (1), March Spec.Issue 2020 Proceedings of the Indian National Science Academy Special Issue : 36th IGC 2020 Geoscience Research in India: The Indian Report to IUGS 2016-2020 (Part II) Guest Editors A K Jain and D M Banerjee Full text available at: http://www.insa.nic.in Proc Indian Natn Sci Acad 86 No. 1 March 2020 pp. 775-875 Printed in India. DOI: 10.16943/ptinsa/2020/49834 The Indian Subcontinent: Its Tectonics A K JAIN1,* and D M BANERJEE2,* CSIR-Central Building Research Institute, Roorkee 247 667, India Department of Geology, University of Delhi, Delhi 110 007, India A new geological and tectonic map of the India Subcontinent is presented with a brief description of its various elements. The map cover parts of India, Bhutan, Nepal, Sri Lanka, Bangladesh, Myanmar, and Pakistan and some of the offshore regions. The Extra-Peninsular region includes the Cenozoic Himalayan Orogen in Pakistan, India Nepal, Bhutan and its possible extension into Myanmar. This belt is separated fronm the Peninsular region by the vast late Cenozoic-Pleistocene Indo-Gangetoc-Brahmaputra Basin. The Peninsular India is mostly composed of six Archean-Proterozoic cratonic nuclei with indications of Hadean elements in Singhbhum. Proterozoic mobile belts surround these nuclei; hence the peninsular part might have been a single continent till end of Proterozoic. Deformation and metamorphism gradually decreased in their intensity, when vast Proterozoic sedimentary basins evolved over the Indian cratons and mobile belts unconformably. Paleo-Mesozoic rifts created the coal-bearing Gondwana basins, followed by marine transgressions before the onset of extensive Deccan volcanic eruptions in the western parts of the continent. -
Newscliping Data English
Environmental Newclipings Data in Newspapers S. No. Volume Date Newspaper Title News Detail 1 6 26-Mar-98 THE INDIAN EXPRESS Development vs displacement: a struggle simmers at Part of Gurez Valley, in north Kashmir along the line of control, an the border ancient tribe is fighting the lone battle against a dam which is considered crucial for the development of the region. In the remote corner of India the valley is the homeland of 25,000 Dard Shin tribes will be submerged once the proposed dam of the Kishen Ganga is built. The land acquisition notices for the Rs.2000 crore 330MW hydro-electric project have already been sent. Dawar, the capital of Gurez and hub of all socio- cultural activity in the area will be drowned and the displacement will not only endanger a language and a particular ethnic community but also their homeland along with the significant archaeological treasure. The government, however, insists that the project is vital for the development of the region and displacement a small price to pay for it and the displaced population will be adequately take care of. 2 6 7-Apr-98 THE FINANCIAL EXPRESS Centre to aid J&Ks revival package for tourism The centre government will give full support to the special packages sector being worked out with leading financial institutions by the Jammu & Kashmir government for revival of the militancy-torn state economy. Leading financial institutions like IFCI, IDBI and many banks will be participating in implementing these packages. The package aims direct finance at subsidised interest rate to entrepreneurs for different categories of tourism activities in the state including that for guest houses, motorboats, travel and excursion and tourist transport. -
GEOGRAPHY Geography Is That Branch of Knowledge- Which Links the Study of Natural World to That of Society
1 GEOGRAPHY Geography is that branch of knowledge- which links the study of natural world to that of society. It is the frame work of various fields of study which cover origin and development of universe, land scapes and its natural environment and pressure created over them, the global and local changes in the world and how and upto what extent the society is contributing in these changes. In this section we are going to cover all these above mentioned aspects in details. Greek Scholar Eratosthenes is first man to discuss about Geography. It’s the combination of two greek words and Geo means earth and graphy” means write. Thus geography means to write about the Earth or “earth descriptions”. Various other geographers defined Geography as follows: In Classical Period (i) Pythagoras, a great Greek philosopher and mathematician, was the first to say that the Earth is spherical and revolves around the sun. (ii) Herodotus Greek historian is known as the “Father of history”. He explained the deposition of silt in the Nile delta. (iii) Aristotle (384 - 322 B.C.) another Greek philosopher explained the eclipses. (iv) Eratosthenes (276 - 194 B.C) a Greek poet, mathematician observing the angle of the noon day Sun at Syene and at Alexandria. (v) Hipparchus (190 - 120 B.C.) was perhaps the greatest of the Greek astronomers. (vi) Ptolemy (2nd century A.D.). He wrote the book ‘Geography’ and he described system of latitudes and longitudes. He was a cartographer and he evolved the science of map-making. Modern Geography 1. Bernhardus Varenius (1622-1650) first recognised the need for organisation of geographical knowledge. -
RELIEF FEATURES of INDIA BY: NEETU SINGH Expanse, Height
RELIEF FEATURES OF INDIA BY: NEETU SINGH Expanse, height and location of India's landforms (plains, plateaus, hills and mountains) have played a significant role not only in influencing her past history but also her climate, land-use, means of transportation and distribution of population, etc. Their study in relation to man and his needs is vital. The following are the four major physiographic divisions of India: (a) A high mountain barrier formed by the Himalayas in the north and the Eastern Highlands also known as Purvachal in the east. (b) The Plains of Northern India or the Great Plains of India (c) The Plateau of Peninsular India, stretching south of the Plains of Northern India (d) The Coastal Lowlands fringing the Plateau of Peninsular India These four regions are distinctly different from one another in respect of their surface configuration. Whereas the Himalayas are young fold mountains with great magnitude of local relief, highly uneven surface, very steep slopes, little level land and young river valleys, the Peninsular India is an old shield block having peneplain areas (due to prolonged erosion), relict mountains and old river valleys. The Plains of Northern India on the other hand are flat and alluvial without any local relief except bluffs of the old banks of the rivers and are of recent origin. The Coastal Lowlands are flat with deltas protruding and land generally rolling. (a) The Himalayas The Himalayas form a highly rugged and continuous stretch of high mountainous country, which flanks northern India for a considerable length and runs between the Brahmaputra Gorge in the east and the Indus in the west.