Mineralogy, Geochemistry and Geochronology of Granitoid Plutons of Dudhi Gneissic Complex, Mahakoshal Belt, Central India
|
|
- Elwin Jackson
- 6 years ago
- Views:
Transcription
1 Mineralogy, Geochemistry and Geochronology of Granitoid Plutons of Dudhi Gneissic Complex, Mahakoshal Belt, Central India Thesis submitted to Kumaun University ar for the requirement of degree of Es t el Doctor of Philosophy in Geology Sita Bora Department of Geology Centre of Advanced Study Kumaun University Nainital July, 2014
2 Dedicated to Parents and Supervisor
3
4
5 Acknowledgments I highly appreciate and grateful, throughout my life, to Dr. R. A. Singh (my teacher) who has introduced and taught Geology during graduation in the year and I consider him founder of the subject Geology to me. I admire him for his valuable advice and career counselling. I extend my sincerest gratitude to all my teachers who gave me strength to make challenging career in the study of rocks during my post-graduation in the year Special and sincerest thanks to Prof. C. C. Pant for his excellent teaching on fundamental aspects and principle of Sedimentology that helped me a lot while understanding and documentation of sedimentary lithounits associated with magmatic bodies in my research area. I always admire and thankful to my teachers Professors A. K. Sharma, G. K. Sharma, R. Upadhyay, P. K. Goswami, B. S. Kotliya and Late S. N. Lal, who taught me all sphere of geology during post-graduation and for their continuous encouragement during the course of present research work. I extend my regards and sincerest thanks to Prof. Anand K. Srivastava who cared and acted as mentor at initial period of my research wok and because of his valuable guidance I was able to trace and reached in the search of magmatic bodies in and around the Renukoot locality of Sonbhadra district of U.P. I am highly indebted to Prof. Santosh Kumar who has not only supervise me but also acted as a founder of Igneous Petrology for me who had introduced and taught us I of igneous petrology which enhanced, replenished, recharged us continuously with knowledge of magmas during the course of research work, and hope we shall always be at receiving end in near future too. Without his inspiration, guidance, motivation and more than that his patient, who is immeasurable, I would have not been able to complete the task in proper way and well in time. I greatly appreciate him for providing me several time opportunities wherever I lost my sincerity. I also express hearty thanks to Dr. Subhra Roy who is truly behind the success of all of us. Because of her real effort, kindness and family-like support, I am able to complete positively the present research work.
6 The journey of the present research work was not so easy, but it became smooth because of moral support rendered by Dr. Rajesh Sharma and Dr. D. R. Rao, who constantly helped and encouraged me while conducting analytical works at Wadia Institute of Himalayan Geology, Dehradun. Dr. Rao has not only helped and guided me during EPMA but also taught about the instrument. I am also thankful to Dr. S. S. Thakur who helped me during EPMA work. I am thankful to Dr. N. K. Saini, Dr. P. P. Khanna for extending analytical helps on XRF and ICP-MS. I am equally thankful to their supporting technical staffmembers Shekhar ji, Rawat ji, Bahuguna ji, Girish ji, Chand Singh ji, D. P. Saklani ji and Mr. Thapliyal ji and many others who directly and indirectly helped me in my research work while my stay at Wadia Institute of Himalayan Geology, Dehradun. I am always thankful to Dr. Umesh K. Sharma, Scientist D, Department of Science and Technology, New Delhi, who encouraged and supported me in every aspect of my research work and continuously motivated me for making career in the field of research. I highly acknowledge the DST-funded project work on CITZ (SR/S4/ES- 402/2009) in which I worked as JRF and SRF and also to Prof. Talat Ahmed (PI of the project) and also to Prof. A. K. Chaudhury, Prof. Sandeep Singh and Prof. R. C. Patel for extending lab facilities for mineral separation at Indian Institute of Technology, Roorkee and Department of Geophysics at Kurukshetra University, Kurukshetra. I deeply acknowledge the DST, New Delhi for International travel support imparting training on SHRIMP at KBSI, Korea. I am highly thankful to Dr. Keewook Yi and Dr. Namhoon Kim at SHRIMP Centre, Korea Basic Science Institute, Korea, who facilitated and introduced me with the advanced technique of Zircon Chronology. They taught and helped me in processing zircon samples and data analysis. They also took care while I was working at SHRIMP centre. Naveen Chauhan and Mukesh, Scientists at KBSI, Korea helped me a lot during my stay at Korea. Tae Ho Lee, Suk_Zu, Shein_a, He_Je, Jeong, Chehang_Park (research students) helped me while analyzing the zircon sample at KBSI, Korea. I am grateful to Dr. V. Balram who provided opportunities to learn geochronology and GCDkit programme that helped me understanding elemental
7 chemistry, modelling and isotope geochemistry. I am thankful to course mentors particularly Prof. Randall R. Parrish, Dr. V. Janousek and Prof. J-F Moyen for imparting training at NGRI, Hyderabad. I am thankful to Dr. S. Raju, Dy Director General, GSI, Chennai for the help procuring geological information on the study area. I also express my deep sense of gratitude to Dr. Brajesh Singh who helped and guided me throughout the research work. I extend my sincere thanks to Manjari Pathak and Ritu Chauhan for their support, help, motivation, and for sparing precious time during the first phase of field investigation. I am very much thankful to Meraj and Naushad for extending help while sampling during third phase of field work in and around Sidhi area, Madhya Pradesh. I also extend my hearty thanks to my all friends especially to Kowete-ü Sekhamo, Samom Jwellys and Mayank Joshi for their concern and support while processing samples at IIT-Roorkee, WIHG and for providing literature. I am thankful to my friends Thomas and Thsope Medo for helping me during analytical works at WIHG, Dehradun. I am thankful to all research scholars at WIHG, Dehradun especially to Sovik and Kaushik for helping me while preparing and polishing the EPMA slides. I extend my sincerest thanks to Maibam Rogibala Di and Ningthoujam Surdas Singh for their support, guidance and care during my stay at Indian Institute of Technology, Roorkee. I am highly thankful to Pramjeet Singh for helping and guiding me during the course of zircon separation at Geophysics Department, Kurukshetra University. I extend my sincere thanks to all the staff member of Department of Geology, Centre of Advanced Study, Kumaun University specially to Ms. R. C. Upadhaya for making excellent thin sections; Bachhi Singh Dhaila for chipping and processing my rock samples; K. D. Mathela, Chandan Singh Dhaila, Harish, Vinod Joshi, Ganga Datt, V. N. Ghoshal, Bhuwan Joshi, Sarvesh ji and Khem Singh for helping me in official works during the entire course of research work. I am highly thankful to Mr. Manohar Singh Rawat, who helped me while compilation of the present work. I express my thanks to all research students of the geology department, particularly to Lalit, Vivekanand, Anoop, Sanjit Kundu, Chitra, Akhre, Harshita, Hansa, Gajendra, Vivek, Saurabh, Laxman and
8
9 Contents Chapter I: Introduction The planet Earth Granite Volcanic-plutonic connexion Granite magmatism in relation to plate tectonics Review of status of knowledge on study area Objectives of present study Chapter II: Geology and Field Relations Introduction Regional geology and tectonics Supracrustal belts Granulite belts Geology of Mahakoshal belt Field observation Harnakachar granitoid (HG) pluton Jhirgadandi granitoid (JG) pluton Asnadhor locality Saliadih locality Jhirgadandi locality Pipraha locality Katoli granitoid (KG) pluton Dudhi granite gneiss Sidhi granitic gneiss Raspahari granitoid (RG) pluton Nerueadamar (NG) and Tumiya (TG) granitoids Volcanics of Mahakoshal Belt Magnetic susceptibility of granitoids and volcanic lithounits... 40
10 Chapter III: Methodology and Instrumentation Techniques Introduction Field Technique Method of sample preparation Microscopic method Magnetic susceptibility Analytical techniques Loss on ignition (LOI) X-ray fluorescence (XRF) spectrometry Inductively coupled plasma mass spectrometry (ICP-MS) U-Th-Pb SHRIMP zircon chronology Analysis of data and used software Chapter IV: Petrography and Mineralogy Introduction Petrography Harnakachar granitoid (HG) pluton Jhirgadanadi granitoid (JG) pluton Katoli granitoid (KG) pluton Dudhi granite gneiss (DG) Raspahari granitoid pluton Nerueadamar (NG) and (TG) Tumiya granitoid plutons Volcanic lithounits Mineral Chemistry Pyroxene Amphibole Classification of amphibole Al-in-amphibole geobarometer Amphibole-plagioclase geothermometer Feldspar Classification of feldspar Feldspar geothermometers
11 Two-feldspar thermometry Single feldspar thermometry Mica Group Biotite chemistry Composition and classification Nature of host granitoid magmas Muscovite chemistry Garnet Chapter V: Geochemistry Introduction Nomenclature Harnakachar granitoid (HG) pluton Jhirgadandi granitoid (JG) pluton Katoli granitoid (KG) pluton Raspahari granitoid (RG) pluton Tumiya (TG) and Nerueadamar (NG) granitoid plutons Volcanic lithounits Major oxide and CIPW norm Harnakachar granitoid (HG) pluton Jhirgadandi granitoid (JG) pluton Katoli granitoid (KG) pluton Dudhi granite gneiss (DG) Raspahari granitoid (RG) pluton Nerueadamar (NG) and Tumiya (TG) granitoid plutons Volcanic lithounits Harker geochemical variation Normalized trace including rare earth elements Harnakachar granitoid (HG) pluton Jhirgadandi granitoid (JG) pluton
12 5.5.3 Katoli granitoid (KG) pluton Dudhi granite gneiss (DG) Raspahari granitoid (RG) pluton Tumiya (TG) and Nerueadamar (NG) granitoid plutons Volcanic lithounits Chapter VI: U-Pb Zircon Chronology Introduction NG pluton: Product of collisional-related thermal event (~1880 Ma) Tumiya pluton: Product of late collisional-related thermal event (~1780 Ma) Vast coeval mafic-felsic magmatism: Major thermal events (~1750 Ma) Jhirgadandi granitoid (JG) Peraluminous microgranular enclave (JE) Metaluminous microgranular enclave (JE) Dudhi granite gneiss (DG) Porphyritic volcanic Coeval mafic-felsic magmatism: minor thermal event (~1730Ma) Katoli granitoid Microgranular enclave (K17E) in KG Age of provenance from quartzite of Harnakachar: evolution of an intra- magmatic or plutonic basin Magmatic event ( ~1710 Ma): HG pluton with older xenolith Chapter VII: Petrogenetic and Geodynamic Discussion Introduction Field evidences Basement of Mahakoshal Belt
13 7.2.2 Evidences of magma intrusion, assimilation, mingling, mixing and undercooling of mafic to hybrid magma globules Magnetite to ilmenite series of granitoids Tectonic scenario and questions remained unanswered Pre to syn sedimentation of magmatism in Mahakoshal Belt Petrographic features of genetic value Crystallization of HG magma and its interaction with enclaves Evidence of JE mingling and syn-crystallization in JG Crystallization of KG magma and its interaction with enclaves Migmatized nature of DG granite gneiss Magmatic processes and protolith assessment of RG pluton Magmatic processes and protolith assessment of NG and TG melts Textural similarities among the granitoid plutons Volcanism and assimilation with country rocks Porphyritic rhyolitic xenoliths in mafic volcanics of Sidhi area: Evidence of fragments of Bundelkhand craton basement Mineral chemical evolution of magmas Nature of JG melt: evidence from pyroxene composition Redox-state of evolving melts under variable P-T conditions: imprinted on amphibole composition Subsolvus granites: evidence from feldspar thermometry Redox conditions of granitoid magmas: evidence from biotite chemistry Water fugacity (ƒh2o) of granitoid melts Tectonic implications: based on biotite chemistry Muscovite composition as an indicator of
14 barren and mineralized granites Geochemical Petrology Granite typology and protolith assessment Depth of granitoid magma emplacement based on normative composition Recognition of magmatic processes Geochemical evolution of HG and HE Mantle derived HG melt fractionation without assimilation Geochemical evolution of JG pluton Mixing between fractionating mafic and felsic magmas Chemically modified JE REE features of mafic and felsic magma fractionation Geochemical evolution of KG pluton Elemental exchange during mingling of mafic-felsic magmas Fractional crystallization (FC): evidence from REE chemistry Geochemical evolution of DG pluton Geochemical evolution of RG pluton Evidence of trace and REE partial equilibration Geochemical evolution of NG and TG plutons Protolith for generation of leucocratic NG and TG melts Low-to-high degree of partial melting Comparison of lithounits with
15 lower, upper and bulk continental crusts Tectonic setting of plutonic and volcanic lithounits Syn-to-post collisional felsic plutonism Fractional crystallization assimilation (AFC) in post-collisional volcanics U-Pb SHRIMP zircon chronology: inferred sequence of geological events Opening of the Mahakoshal Basin: evidence from inherited and magmatic zircons of NG and TG plutons Slow rate of Mahakoshal Basin closure: evidence from collisional-related plutonism Bimodal mafic-felsic magmatism in post-collision tectonic setting Coeval mafic-felsic magma interaction in plutonic setting Intra-plutonic sedimentation A viable model for the evolution of Mahakoshal Belt Comparison of past Mahakoshal orogeny with present younger Himalayan orogeny in Indian subcontinent Chapter VIII: Summary and Conclusions References
Estelar. Summary and Conclusions. Chapter VIII
Chapter VIII Summary and Conclusions The E-W trending Central Indian Tectonic Zone (CITZ) divides the Peninsular India into northern Bundelkhand craton and southern Bastar, Dharwar, Singhbhum cratons.
More informationSociety of Earth Scientists Series
Society of Earth Scientists Series Series editor Satish C. Tripathi, Lucknow, India For further volumes: http://www.springer.com/series/8785 The Society of Earth Scientists Series aims to publish selected
More informationThis file is part of the following reference: Access to this file is available from:
ResearchOnline@JCU This file is part of the following reference: Hoadley, Elizabeth (2003) Evolution of the Sybella Batholith: Petrographic, geochemical and structural development of an A-type intrusive
More informationClassification and Origin of Granites. A Multi-faceted Question
Classification and Origin of Granites A Multi-faceted Question What is a granite? IUGS classification Based on Modal Mineralogy Plutonic rock with less than 90% mafic minerals Alkali Granite Granite Quartz
More informationDUST EXPLOSION MODELING USING MECHANISTIC AND PHENOMENOLOGICAL APPROACHES
DUST EXPLOSION MODELING USING MECHANISTIC AND PHENOMENOLOGICAL APPROACHES VIMLESH KUMAR BIND DEPARTMENT OF CHEMICAL ENGINEERING Submitted in fulfillment of the requirements of the degree of DOCTOR OF PHILOSOPHY
More informationStudent Name: College: Grade:
Student Name: College: Grade: Physical Geology Laboratory IGNEOUS MINERALS AND ROCKS IDENTIFICATION - INTRODUCTION & PURPOSE: In this lab you will learn to identify igneous rocks in hand samples from their
More informationPETROGENESIS OF A GRANITE XENOLITH IN THE 1.1 GA MIDCONTINENT RIFT AT SILVER BAY, MN
PETROGEESIS OF A GRAITE XEOLITH I THE 1.1 GA MIDCOTIET RIFT AT SILVER BAY, M ATALIE JUDA Macalester College Sponsor: Karl Wirth ITRODUCTIO Much of the study of the orth American 1.1 Ga Keweenawan Midcontinent
More informationCURRICULUM-VITAE. Correspondence: Dept. of Geology, AMU, Aligarh
CURRICULUM-VITAE 1. Name : Dr. SHAIK ABDUL RASHID 2. Present Status Working as Associate Professor in the Department of Geology, Aligarh Muslim University, Aligarh, India for the last 16 years and teaching
More informationPLATE TECTONICS, VOLCANISM AND IGNEOUS ROCKS
PLATE TECTONICS, VOLCANISM AND IGNEOUS ROCKS PLATE TECTONICS TO IGNEOUS ROCKS Internal Heat Seafloor Spreading/Plate Tectonics Volcanism Plate Boundary Intra-plate (hot spot) Divergent Convergent Igneous
More informationACADEMIC PROFILE OF FACULTY MEMBER 1. Name: Santosh Kumar 2. Designation: Professor 3. Qualification: B.Sc., M.Sc. (Geography: Land & Water
ACADEMIC PROFILE OF FACULTY MEMBER 1. Name: Santosh Kumar 2. Designation: Professor 3. Qualification: B.Sc., M.Sc. (Geography: Land & Water Resources), M.Sc. (Geology), P.G. Diploma (Spectroscopy), Ph.D.
More informationLecture 3 Rocks and the Rock Cycle Dr. Shwan Omar
Rocks A naturally occurring aggregate of one or more minerals (e.g., granite), or a body of non-crystalline material (e.g., obsidian glass), or of solid organic material (e.g., coal). Rock Cycle A sequence
More informationIgneous Rocks. Igneous Rocks - 1. Environment of Formation - Magma - Plutonic - rock that formed within the Earth. Intrusive - Earth s crust.
Name: Date: Period: Minerals and Rocks The Physical Setting: Earth Science CLASS NOTES - Methods to classify igneous rocks: 1. Environment of Formation - Magma - Plutonic - rock that formed within the
More informationEngineering Geology ECIV 2204
Engineering Geology ECIV 2204 Instructor : Dr. Jehad Hamad 2017-2016 Chapter (3) Igneous Rocks Chapter 3: Rocks: Materials of the Solid Earth Igneous Rocks Chapter 3: Rocks: Materials of the Solid Earth
More informationCarbonatites to Alkali Granites Petrogenetic Insights from the Chilwa and Monteregian Hills-White Mountain Igneous Provinces
Carbonatites to Alkali Granites Petrogenetic Insights from the Chilwa and Monteregian Hills-White Mountain Igneous Provinces G. Nelson Eby Department of Environmental, Earth, & Atmospheric Sciences University
More informationIgneous Rock Classification, Processes and Identification Physical Geology GEOL 100
Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100 Ray Rector - Instructor Major Concepts 1) Igneous rocks form directly from the crystallization of a magma or lava 2)
More informationESS103A Igneous Petrology
Welcome to ESS103A Igneous Petrology Please pick up handouts Plan for today: Who are we? What is this class about? What is the structure of this course? How does the scientific method work? Who are we?
More informationIgneous and Metamorphic Rock Forming Minerals. Department of Geology Mr. Victor Tibane SGM 210_2013
Igneous and Metamorphic Rock Forming Minerals Department of Geology Mr. Victor Tibane 1 SGM 210_2013 Grotzinger Jordan Understanding Earth Sixth Edition Chapter 4: IGNEOUS ROCKS Solids from Melts 2011
More informationIMSG Post-conference Field Guide
IMSG 2017 - Post-conference Field Guide Jérémie Lehmann, Marlina Elburg and Trishya Owen-Smith The purpose of this short field excursion on Wednesday 18 January is to show a variety of rocks that make
More informationINTRODUCTION ROCK COLOR
LAST NAME (ALL IN CAPS): FIRST NAME: 6. IGNEOUS ROCKS Instructions: Some rocks that you would be working with may have sharp edges and corners, therefore, be careful when working with them! When you are
More informationPETROGENESIS OF ENCLAVES WITHIN THE PEGGY S COVE MONZOGRANITE, SOUTHERN NOVA SCOTIA, CANADA
PETROGENESIS OF ENCLAVES WITHIN THE PEGGY S COVE MONZOGRANITE, SOUTHERN NOVA SCOTIA, CANADA HINA IMTIAZ Trinity University Research Advisor: Dr. Benjamin Surpless INTRODUCTION The Canadian province of
More informationPlate tectonics, rock cycle
Dikes, Antarctica Rock Cycle Plate tectonics, rock cycle The Rock Cycle A rock is a naturally formed, consolidated material usually composed of grains of one or more minerals The rock cycle shows how one
More informationPage 1. Name:
Name: 1) What is the approximate density of a mineral with a mass of 262.2 grams that displaces 46 cubic centimeters of water? A) 6.1 g/cm 3 C) 1.8 g/cm 3 B) 5.7 g/cm 3 D) 12.2 g/cm 3 2) In which two Earth
More informationEARTH SCIENCE. Geology, the Environment and the Universe. Chapter 5: Igneous Rocks
EARTH SCIENCE Geology, the Environment and the Universe Chapter 5: Igneous Rocks CHAPTER 5 Igneous Rocks Section 5.1 What are igneous rocks? Section 5.2 Classification of Igneous Rocks Click a hyperlink
More informationRocks: Materials of the Solid Earth
1 Rocks: Materials of the Solid Earth Presentation modified from: Instructor Resource Center on CD-ROM, Foundations of Earth Science,, 4 th Edition, Lutgens/Tarbuck, Rock Cycle Igneous Rocks Today 2 Rock
More informationLecture 5 Sedimentary rocks Recap+ continued. and Metamorphic rocks!
Lecture 5 Sedimentary rocks Recap+ continued and Metamorphic rocks! Metamorphism Process that leads to changes in: Mineralogy Texture Sometimes chemical composition Metamorphic rocks are produced from
More informationGeochemical Characterization of Schirmacher Orthogneiss, Schirmacher Oasis, CDML, East Antarctica
Twentieth Indian Expedition to Antarctica, Scientific Report, 2006 Ministry of Earth Sciences, Technical Publication No. 18, pp 147-164 Geochemical Characterization of Schirmacher Orthogneiss, Schirmacher
More informationGEOL Lab 11 (Metamorphic Rocks in Hand Sample and Thin Section)
GEOL 333 - Lab 11 (Metamorphic Rocks in Hand Sample and Thin Section) Introduction - Metamorphic rock forms from any pre-existing rock that undergoes changes due to intense heat and pressure without melting.
More informationIgneous Rocks. Sedimentary Rocks. Metamorphic Rocks
Name: Date: Igneous Rocks Igneous rocks form from the solidification of magma either below (intrusive igneous rocks) or above (extrusive igneous rocks) the Earth s surface. For example, the igneous rock
More informationHow does the mantle beneath the Ring of Fire change through time?: a trace element
Page 1 How does the mantle beneath the Ring of Fire change through time?: a trace element study of primitive basalts erupted in a small area in the Southern Cascades Abstract I will test the hypothesis
More informationLisa Gaston NMT. Photo courtesy of Mike Williams. Matt Heizler
Lisa Gaston NMT Photo courtesy of Mike Williams Matt Heizler Precambrian Geology Field Area 40 Ar/ 39 Ar results Do the pegmatites record intrusion ages? Conclusions Future work Precambrian provinces of
More informationGEOLOGY - Granitoid Evolution and Tectonic History of the Central Asian Orogenic Belt in Northeast China
GEOLOGY - Granitoid Evolution and Tectonic History of the Central Asian Orogenic Belt in Northeast China Title Summary of Proposed Research Program for Doctor of Philosophy Granitoid Evolution and Tectonic
More informationGY 112 Lecture Notes Archean Geology
GY 112 Lecture Notes D. Haywick (2006) 1 GY 112 Lecture Notes Archean Geology Lecture Goals: A) Time frame (the Archean and earlier) B) Rocks and tectonic elements (shield/platform/craton) C) Tectonics
More informationCOURSE INFORMATION. NAME OF THE SUBJECT: Petrology of igneous and metamorphic rocks TEACHING STAFF
COURSE INFORMATION NAME OF THE SUBJECT: Petrology of igneous and metamorphic rocks Code number: 757609217 Degree in Geology Academic Year: 2016-2017 Foundational/Elective/Compulsory course. 3 rd year Second
More informationGLY 155 Introduction to Physical Geology, W. Altermann. Grotzinger Jordan. Understanding Earth. Sixth Edition
Grotzinger Jordan Understanding Earth Sixth Edition Chapter 4: IGNEOUS ROCKS Solids from Melts 2011 by W. H. Freeman and Company Chapter 4: Igneous Rocks: Solids from Melts 1 About Igneous Rocks Igneous
More informationPetrology and Geochronology of Iran Tepe volcano, Eastern Rhodopes, Bulgaria: Age relationship with the Ada Tepe gold deposit. (preliminary data)
Petrology and Geochronology of Iran Tepe volcano, Eastern Rhodopes, Bulgaria: Age relationship with the Ada Tepe gold deposit. (preliminary data) Peter Kibarov, Peter Marchev, Maria Ovtcharova, Raya Raycheva,
More informationEssentials of Geology, 11e
Essentials of Geology, 11e Igneous Rocks and Intrusive Activity Chapter 3 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois College Characteristics
More informationAN OXYGEN ISOTOPE STUDY ON THE ORIGINS OF GARNET IN THE PERALUMINOUS SOUTH MOUNTAIN BATHOLITH, NOVA SCOTIA
AN OXYGEN ISOTOPE STUDY ON THE ORIGINS OF GARNET IN THE PERALUMINOUS SOUTH MOUNTAIN BATHOLITH, NOVA SCOTIA JESSICA HARK College of Wooster Sponsor: Jade Star Lackey INTRODUCTION Nova Scotia represents
More informationFigure 2.2a. A classification of the phaneritic igneous rocks: Phaneritic rocks with more than 10% (quartz +
Granitoids Figure 2.2a. A classification of the phaneritic igneous rocks: Phaneritic rocks with more than 10% (quartz + feldspar + feldspathoids). After IUGS. Winter (2001) An Introduction to Igneous and
More informationMetamorphic Energy Flow. Categories of Metamorphism. Inherited Protolith Character. Inherited Fabric. Chemical Composition
Metamorphic Energy Flow Categories of Metamorphism Best, Chapter 10 Metamorphic processes are endothermic They absorb heat and mechanical energy Absorption of heat in orogenic belts Causes growth of mineral
More informationMetamorphic Rock Origin and Identification
Metamorphic Rock Origin and Identification Physical Geology GEOL 101 Lab Ray Rector - Instructor http://www.rockhounds.com/rockshop/rockkey/index.html http://earthsci.org/education/teacher/basicgeol/meta/meta.html
More informationFACTS FOR DIAMOND OCCURRENCE IN KIMBERLITES
KIMBERLITES Kimberlite is an ultrabasic olivine-rich igneous rock called peridotite. Peridotites occur at great depths in the earth in a layer called the mantle (100-135 miles below the surface). At this
More informationGeochemical Characteristics of the Charnockitic and Associated Granitic Rock, Akure Area, Southwestern Nigeria.
Geochemical aracteristics of the arnockitic and Associated Granitic Rock, Akure Area, Southwestern Nigeria. Ademeso Odunyemi Anthony *, Alabi Kayode,. Department of Geology, Adekunle Ajasin University,
More informationLab 6: Metamorphic Rocks
Introduction The Earth s crust is in a constant state of change. For example, plutonic igneous rocks are exposed at the surface through uplift and erosion. Many minerals within igneous rocks are unstable
More informationMetamorphic Rock Origin and Identification
Metamorphic Rock Origin and Identification Geology Laboratory GEOL 101 Lab Ray Rector - Instructor http://www.rockhounds.com/rockshop/rockkey/index.html http://earthsci.org/education/teacher/basicgeol/meta/meta.html
More informationMagma fertility: Concepts and JCU research at NQ
Magma fertility: Concepts and JCU research at NQ Zhaoshan Chang*, Carl Spandler, Yanbo Cheng EGRU, JCU *Zhaoshan.chang@jcu.edu.au 27 May 2015 Townsville, Queensland, Australia Magma fertility Miners dream
More informationGEOL FORENSIC GEOLOGY ROCK IDENTIFICATION
GEOL.2150 - FORENSIC GEOLOGY ROCK IDENTIFICATION Name I. Introduction There are three basic types of rocks - igneous, sedimentary, and metamorphic: Igneous. Igneous rocks have solidified from molten matter
More informationMetamorphic Petrology GLY 262 P-T-t paths
Metamorphic Petrology GLY 262 P-T-t paths Pressure-Temperature-Time (P-T-t) Paths The complete set of T-P conditions that a rock may experience during a metamorphic cycle from burial to metamorphism (and
More informationChapter 4 Rocks & Igneous Rocks
Chapter 4 Rocks & Igneous Rocks Rock Definition A naturally occurring consolidated mixture of one or more minerals e.g, marble, granite, sandstone, limestone Rock Definition Must naturally occur in nature,
More informationGEOLOGY. Subject : GEOLOGY (For under graduate student.) Paper No. : Paper 02 Introduction to Geology 02
GEOLOGY Subject : GEOLOGY (For under graduate student.) Paper No. : Paper 02 Introduction to Geology 02 Topic No. & Title : 37 Magma Bowen Series (Part 01) Academic Script What is Igneous Petrology? Igneous
More informationRocks Rock- A group of minerals, glass, mineroid bound together in some way.
Rocks Rock- A group of minerals, glass, mineroid bound together in some way. All rocks fit into one of three categories: Igneous- formed by the cooling and hardening of hot molten rock Sedimentary- formed
More informationIGNEOUS ROCKS. SECTION 5.1 What are igneous rocks?
Date Period Name IGNEOUS ROCKS SECTION.1 What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. basaltic
More informationTo get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle
To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle Bell Ringer Name the 3 types of rock. Is one type of rock able to change into a different
More informationSoil Mechanics/Geotechnical Engineering I Prof. Dilip Kumar Baidya Department of Civil Engineering Indian Institute of Technology, Kharagpur
Soil Mechanics/Geotechnical Engineering I Prof. Dilip Kumar Baidya Department of Civil Engineering Indian Institute of Technology, Kharagpur Lecture - 01 Rock Cycle Good morning. I welcome you to this
More informationpredictive iscovery Why is the gold where it is? redictive mineral ineral discovery pmd CRC
The Y2 project (2001-2004) Time-space evolution of the Yilgarn Craton: implications for geodynamics Kevin Cassidy and the Y2 team Reduced D Risk through Improved Targeting ineral d Why is the gold where
More informationLab: Metamorphism: minerals, rocks and plate tectonics!
Introduction The Earth s crust is in a constant state of change. For example, plutonic igneous rocks are exposed at the surface through uplift and erosion. Many minerals within igneous rocks are unstable
More information6. IGNEOUS ROCKS AND VOLCANIC HAZARDS
LAST NAME (ALL IN CAPS): FIRST NAME: 6. IGNEOUS ROCKS AND VOLCANIC HAZARDS Instructions: Refer to Laboratory 5 in your lab book on pages 129-152 to answer the questions in this work sheet. Your work will
More informationDr. Ashwini Kumar Choudhary Professor Institute Instrumentation Center Indian Institute of Technology, Roorkee Roorkee , India
1 Dr. Ashwini Kumar Choudhary Professor Institute Instrumentation Center Indian Institute of Technology, Roorkee Roorkee - 247667, India Date of Birth: 19 September 1949 Office Tel: +91-1332-285148 E-mail:
More informationThe 3 types of rocks:
Igneous Rocks and Intrusive Igneous Activity The 3 types of rocks:! Sedimentary! Igneous! Metamorphic Marble 1 10/7/15 SEDIMENTARY ROCKS Come from rocks sediments (rock fragments, sand, silt, etc.) Fossils
More informationRAYMOND SIEVER Harvard University
E A R T H FOURTH EDITION FRANK PRESS National Academy of Sciences RAYMOND SIEVER Harvard University W. H. Freeman and Company New York Preface xiii Acknowledgments xviii PART I PROLOGUE CHAPTER 1 HISTORY
More informationImagine the first rock and the cycles that it has been through.
A rock is a naturally formed, consolidated material usually composed of grains of one or more minerals The rock cycle shows how one type of rocky material gets transformed into another The Rock Cycle Representation
More informationCLASSIFICATION OF ANTARCTIC TILL COBBLES THROUGH GEOCHEMICAL ANALYSIS & COMPARISON
CLASSIFICATION OF ANTARCTIC TILL COBBLES THROUGH GEOCHEMICAL ANALYSIS & COMPARISON Rachel Powers & Felix Zamora NDSU GEOL 422 May, 2012 Study Area Transantarctic Mountains Study Area Friis Hills, Southern
More informationPractice Test Rocks and Minerals. Name. Page 1
Name Practice Test Rocks and Minerals 1. Which rock would be the best source of the mineral garnet? A) basalt B) limestone C) schist D) slate 2. Which mineral is mined for its iron content? A) hematite
More informationNeoproterozoic Malani Magmatism, northwestern Indian shield: Not a plume product. Kamal K. Sharma
Neoproterozoic Malani Magmatism, northwestern Indian shield: Not a plume product Kamal K. Sharma Department of Geology, Government Postgraduate College, Sirohi (Rajasthan) 307001 India sharmasirohi@yahoo.com
More informationName Class Date STUDY GUIDE FOR CONTENT MASTERY
Igneous Rocks What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. extrusive igneous rock intrusive
More informationFluorine and Chlorine in Alkaline Rocks and A-type Granites
Fluorine and Chlorine in Alkaline Rocks and A-type Granites Using the fluorine and chlorine content of Amphibole, Apatite and Biotite to monitor magma halogen content Chilwa Province, Malawi, and Carboniferous
More informationReview - Unit 2 - Rocks and Minerals
Review - Unit 2 - Rocks and Minerals Base your answers to questions 1 and 2 on the diagram below, which shows the results of three different physical tests, A, B, and C, that were performed on a mineral.
More informationPETROGENESIS OF A SERIES OF MAFIC SHEETS WITHIN THE VINALHAVEN PLUTON, VINALHAVEN ISLAND, MAINE
PETROGENESIS OF A SERIES OF MAFIC SHEETS WITHIN THE VINALHAVEN PLUTON, VINALHAVEN ISLAND, MAINE DANIEL HAWKINS Western Kentucky University Research Advisor: Andrew Wulff INTRODUCTION Round Point, in the
More informationCHAPTER 3.3: METAMORPHIC ROCKS
CHAPTER 3.3: METAMORPHIC ROCKS Introduction Metamorphism - the process of changes in texture and mineralogy of pre-existing rock due to changes in temperature and/or pressure. Metamorphic means change
More informationLin Chen Robert A Creaser Daniel J Kontak Oct 29th, 2014
FURTHER Re-Os ARSENOPYRITE GEOCHRONOLOGY FROM SELECTED MEGUMA AU DEPOSITS, MEGUMA TERRANE, NOVA SCOTIA: POSSIBLE EVIDENCE FOR A PROTRACTED GOLD-FORMING SYSTEM Lin Chen Robert A Creaser Daniel J Kontak
More informationDirected Reading. Section: Rocks and the Rock Cycle. made of a. inorganic matter. b. solid organic matter. c. liquid organic matter. d. chemicals.
Skills Worksheet Directed Reading Section: Rocks and the Rock Cycle 1. The solid part of Earth is made up of material called a. glacial ice. b. lava. c. rock. d. wood. 2. Rock can be a collection of one
More informationPetrography and Magnetic Investigation of Western Part of Zafarghand Granitoidic Pluton, Ardestan, Isfahan.
Petrography and Magnetic Investigation of Western Part of Zafarghand Granitoidic Pluton, Ardestan, Isfahan. Corresponding authors: Negar Gavanji*, Dr.Mahmood sadeghian. Postal address: Iran, Shahrood,
More informationCHAPTER VI CONCLUSIONS
CHAPTER VI CONCLUSIONS In this Chapter, salient observations made in understanding the various tectonothermal events, including U-Pb in-situ monazite geochronology of Sargur schists and granulites exposed
More informationUNIVERSITY OF CALCUTTA
UNIVERSITY OF CALCUTTA FACULTY ACADEMIC PROFILE/ CV 1. Full name of the faculty member: Dr. BAPI GOSWAMI 2. Designation: ASSOCIATE PROFESSOR 3. Specialisation: PETROLOGY, GEOCHEMISTRY 4. Passport size
More informationObjectives of this Lab. Introduction. The Petrographic Microscope
Geological Sciences 101 Lab #9 Introduction to Petrology Objectives of this Lab 1. Understand how the minerals and textures of rocks reflect the processes by which they were formed. 2. Understand how rocks
More informationUnit 2 Exam: Rocks & Minerals
Name: Date: 1. Base your answer(s) to the following question(s) on the 2001 edition of the Earth Science Reference Tables, the map and cross section below, and your knowledge of Earth science. The shaded
More informationLecture 6 - Igneous Rocks and Volcanoes
Lecture 6 - Igneous Rocks and Volcanoes Learning objectives Understand and be able to predict where and why magma will be forming at different tectonic settings Understand the factors controlling magma
More informationThe Lead 206/207 Dating Method
The Lead 206/207 Dating Method 1 U Pb Zircon Ages, Chemical Geology, Volume 211 (2004) Pages 87 109 2 Lead Isotope Planetary Profiling, Chemical Geology, Volume 233 (2006) Pages 1 45 3 U Pb Step-Leaching
More informationMetamorphism: Alteration of Rocks by Temperature and Pressure
CHAPTER 6 Metamorphism: Alteration of Rocks by Temperature and Pressure Chapter Summary Metamorphism is the alteration in the solid state of preexisting rocks, including older metamorphic rocks. Increases
More informationGeochemistry of Mafic Dykes of Chittoor District, Andhra Pradesh, Southern India
http://www.e-journals.in Chemical Science Transactions DOI:10.7598/cst2014.822 2014, 3(3), 953-960 RESEARCH ARTICLE Geochemistry of Mafic Dykes of Chittoor District, Andhra Pradesh, Southern India D. B.
More information2 Britain s oldest rocks: remnants of
Britain s oldest rocks: remnants of Archaean crust 15 2 Britain s oldest rocks: remnants of Archaean crust 2.1 Introduction Owing to the complex nature of extremely old deformed rocks, the standard methods
More informationMATHEMATICAL MODELLING OF DISPERSION OF AIR POLLUTANTS IN LOW WIND CONDITIONS
MATHEMATICAL MODELLING OF DISPERSION OF AIR POLLUTANTS IN LOW WIND CONDITIONS by ANIL KUMAR YADAV Thesis submitted to the Indian Institute of Technology, Delhi for the award of the degree of DOCTOR OF
More informationPage 1. Name: 1) Which diagram best shows the grain size of some common sedimentary rocks?
Name: 1) Which diagram best shows the grain size of some common sedimentary rocks? 1663-1 - Page 1 5) The flowchart below illustrates the change from melted rock to basalt. 2) Which processes most likely
More informationThe Geochemistry of Basalts in northeast of Darood Neyshaboor, NE Iran
The Geochemistry of asalts in northeast of Darood Neyshaboor, NE Iran Mehdi rbabi Tehran 1, H. Mehdizadeh Shahri 2, M. E. Fazel Valipour 3 1) Islamic zad University of Shahrood, Department of Geology 2)
More informationChapter 4 8/27/2013. Igneous Rocks. and Intrusive Igneous Activity. Introduction. The Properties and Behavior of Magma and Lava
Introduction Chapter 4 Igneous rocks form by the cooling of magma (or lava). Large parts of the continents and all the oceanic crust are composed of. and Intrusive Igneous Activity The Properties and Behavior
More informationEarth Science 232 Petrography
Earth Science 232 Petrography Course notes by Shaun Frape and Alec Blyth Winter 2002 1 Petrology - Introduction Some Definitions Petra Greek for rock Logos Greek for disclosure or explanation Petrology
More informationChapter IV MINERAL CHEMISTRY
Chapter IV MINERAL CHEMISTRY Chapter-IV MINERAL CHEMISTRY 4.1 INTRODUCTION In this chapter, chemical analyses of different minerals present in various rocks of Mashhad granitoid plutons have been presented.
More information6 Exhumation of the Grampian
73 6 Exhumation of the Grampian mountains 6.1 Introduction Section 5 discussed the collision of an island arc with the margin of Laurentia, which led to the formation of a major mountain belt, the Grampian
More informationMetcalf and Buck. GSA Data Repository
GSA Data Repository 2015035 Metcalf and Buck Figure DR1. Secondary ionization mass-spectrometry U-Pb zircon geochronology plots for data collected on two samples of Wilson Ridge plutonic rocks. Data presented
More informationName. GEOL.3250 Geology for Engineers Igneous Rocks
Name GEOL.3250 Geology for Engineers Igneous Rocks I. Introduction The bulk of the earth's crust is composed of relatively few minerals. These can be mixed together, however, to give an endless variety
More informationPETROLOGY OF A SYSTEM OF GRANOPHYRE DIKES IN THE BEAVER BAY COMPLEX IN BEAVER BAY, MINNESOTA
PETROLOGY OF A SYSTEM OF GRANOPHYRE DIKES IN THE BEAVER BAY COMPLEX IN BEAVER BAY, MINNESOTA MATT ANDRING Whitman College Sponsor: John Winter INTRODUCTION The Beaver Bay Complex is an intrusive igneous
More informationGEOLOGY - Tectonic Setting and Tectonometamorphic Evolution of Fuping-Wutai- Hengshan Orogenic Belt, China
GEOLOGY - Tectonic Setting and Tectonometamorphic Evolution of Fuping-Wutai- Hengshan Orogenic Belt, China Title Summary of Proposed Research Program for Doctor of Philosophy Tectonic Setting and Tectonometamorphic
More informationFiled and Textural Evidences of Magma Mingling Recorded in the Tekyeh-Bala Area Granitoid Rocks, Southeast of the Kordestan Province, West Iran
Australian Journal of Basic and Applied Sciences, 5(12): 1513-1517, 2011 ISSN 1991-8178 Filed and Textural Evidences of Magma Mingling Recorded in the Tekyeh-Bala Area Granitoid Rocks, Southeast of the
More informationTHE CONTAMINATION HISTORY OF THE BOOT LAKE GRANODIORITE, NOVA SCOTIA
THE CONTAMINATION HISTORY OF THE BOOT LAKE GRANODIORITE, NOVA SCOTIA BRIAN MUMAW College of Wooster Sponsor: Jade Star Lackey INTRODUCTION The Boot Lake Granodiorite is a strongly peraluminous pluton (Al
More informationEASC100: EXAM1 (07) Lithosphere and Hydrosphere
EASC100: EXAM1 (07) Lithosphere and Hydrosphere Name: 1. Why do Mercury and the Moon lack an atmosphere? A) They formed after all the gas had been used up. B) They are so cold that all their gases have
More informationGeological Studies in the Larsemann Hills, Ingrid Chirstensen Coast, East Antarctica
363 Twenty Fourth Indian Antarctic Expedition 2003-2005 Ministry of Earth Sciences, Technical Publication No. 22, pp 363-367 Geological Studies in the Larsemann Hills, Ingrid Chirstensen Coast, East Antarctica
More informationCAMBRIAN INTRUSION-RELATED COPPER MINERALISATION AT THE THOMAS CREEK PROSPECT, SOUTHWESTERN TASMANIA
CAMBRIAN INTRUSION-RELATED COPPER MINERALISATION AT THE THOMAS CREEK PROSPECT, SOUTHWESTERN TASMANIA UN I VF.RS TTY OF TASMANIA By Robert Reid (B.Sc. Hons) A thesis submitted in partial fulfillment of
More informationChapter 10. Chapter Rocks and the Rock Cycle. Rocks. Section 1 Rocks and the Rock Cycle
Chapter 10 Rocks 1 Chapter 10 Section 1 Rocks and the Rock Cycle 2 10.1 Rocks and the Rock Cycle Magma is the parent material for all rocks. Once the magma cools and hardens, many changes can occur. Geology:
More informationCHAPTER 8 SUMMARY AND CONCLUSIONS
CHAPTER 8 SUMMARY AND CONCLUSIONS The Aravalli Mountain Range (AMR) is the main edifice of NW Indian shield. It is about 800 km long and 200 km wide with NE-SW strike. The rocks of AMR are hosted in an
More informationEstelar. Introduction
Chapter-1 Granitic magmas only occur in volume where a thick crust, old or new, can provide a fertile source, a thermal blanket and sufficient space for differentiation processes to operate. 1.1 Wallace
More informationArchean Terranes. Archean Rocks. Southeastern Africa. West Greenland. Kaapvaal Craton. Ancient Gneiss Complex
Archean Terranes Archean Rocks Chapter 15A >2.5 Gy old Younger supracrustal sequences Greenstone belts Calc-alkaline metavolcanic rocks Older gneiss complexes Quartzo-feldspathic rocks Tonalites and migmatites
More information