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K Feldspar from
Panwad-Kawant, Chhota Udaipur District, Gujarat, India


Locality type:Complex
Classification
Species:'K Feldspar' (not an IMA approved species)
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view K Feldspar data
Locality Data:Click here to view Panwad-Kawant, Chhota Udaipur District, Gujarat, India
Data Identifiers
Mindat Occurrence Record ID:1332397
Long-form Identifier:1:3:1332397:4
GUID (UUID V4):4c389a39-438f-4c11-a37f-6f54e31280bd
Nearest other occurrences of K Feldspar
3.9km (2.4 miles) Siriwasan-Dughda, Chhota Udaipur District, Gujarat, India
6.7km (4.2 miles) Amba Dongar complex, Chhota Udaipur District, Gujarat, India
6.9km (4.3 miles) Ambadungar, Chhota Udaipur District, Gujarat, India
References
Reference Search (possible matching items)
Journal (article/letter/editorial)
and Adjacent Areas, Deccan Igneous Province, Gujarat, India: 1. Geology, Petrography and Petrochemistry...intrusions cover ~ 1200 km 2 south of the town of Chhota Udaipur, and form a subprovince within the alkaline...tholeiitic gabbro-granophyre intrusion); (4) Panwad-Kawant: dykes and plugs of lamprophyres and tephrites...higher incompatible and LIL element contents (Rb, K, Nb, Zr, Sr, Ba, LREE, etc.) than the associated tholeiites...yon Amba Dongar und Umgebung, Dekkan-Provinz, Gujarat, Indien: 1. Geologic, Petrographic und Gesteinschemie
Journal (article/letter/editorial)
The Origin of Pseudoleucite in Tinguaite, Ghori, India: a Reevaluation1 S. G. Viladkar Emeritus, Geology...Research Centre, Amba Dongar Kadipani, District Vadodara, India390117 email: sviladkar@gmail.com Received...Ghori which is located in the PanwadKawant carbonatitealkalic complex, India. In thin sections the pseudoleucite...attributed to an inter growth assemblage of Kfeldspar + nepheline after primary leucite. Many publications...pseudoleucite in India was first reported from a tinguaite dykes at Ghori (Fig. 1), Chhota Udaipur, Gujarat by Sukheswaia
Journal (article/letter/editorial)
South America and India. In the Indian Subcontinent carbonatites occur in India, Pakistan, Afghanistan...considerable time range (>2400 Ma to <0.6 Ma) from India (Hogenakal, Newania, Sevathur, Sung Valley, Sarnu-Dandali...Geology, RTM Nagpur University, Nagpur (MH) – 440001, India; Email: randive101@yahoo.co.in Tushar Meshram: Department...440001, India; Geological Survey of India, Central Region, Seminary Hills, Nagpur (MH) – 440006, India Open...Open Access. © 2020 K. Randive and T. Meshram, published by De Gruyter. Attribution 4.0 License Keywords:
Journal (article/letter/editorial)
Pande & S. K. Pattanayak To cite this article: Jyotiranjan S. Ray , Kanchan Pande & S. K. Pattanayak...PANDE, AND S. K. PATTANAYAK Physical Research Laboratory, Navrangpura, Ahmedabad 380 009, India Downloaded...within the Chhota Udaipur subprovince of the Deccan flood basalt province, western India. Despite previous...view that all the alkaline activity in the Chhota Udaipur subprovince was contemporaneous. This in turn...The Deccan flood basalt province of west-central India is one of the world’s major Phanerozoic CFB provinces
Book
Series Series Editor Satish C. Tripathi, Lucknow, India The Society of Earth Scientists Series aims to...Atmospheric Science University of Hyderabad Hyderabad, India ISSN 2194-9204 ISSN 2194-9212 (electronic) Society...Gewerbestrasse 11, 6330 Cham, Switzerland Foreword India is known since long to possess large reserves of...rich in light rare earth element. Exploration in India for Rare Earth Element (REE) deposits since the...the RE Industry in India largely through the initiative taken by the IREL (India) Limited, the Atomic
Journal (article/letter/editorial)
geochemistry and K–Ar ages for Cenozoic tinguaites from the Ohře/Eger Rift (NW Bohemia) J. Ulrych, J. K. Novák...Novák, M. Lang, Praha, K. Balogh, Debrecen, E. Hegner, München, and Z. Řanda, Řež With 11 figures and 11...patterns interstitially in a mosaic of alkali feldspar and foids) phonolites, hereafter referred to as...crustal levels with limited assimilation of crust. K–Ar ages of 31– 28.5 Ma for five samples suggest that...the first K–Ar data reported by Ulrych & Balogh (2000) probably due to disturbance of the K–Ar isotopic
Book
Institute of Technology Bombay Mumbai, Maharashtra, India ISBN 978-3-319-67704-0    ISBN 978-3-319-67705-7...the Physical Research Laboratory (PRL, Ahmedabad, India), the National Autonomous University of Mexico (UNAM)...Geoscience Award of the Ministry of Mines, Govt. of India (2010), and the M. R. Srinivasa Rao Award in Petrology...Petrology of the Geological Society of India (2017). His major research interests are flood basalt volcanism...Natural Gas Corporation (ONGC), Sundargarh, Odisha, India e-mail: ali_md2@ongc.co.in Carla Joana Santos Barreto
Book
Northwestern United States Richard W. Carlson and William K. Hart 35 The Ethiopian Flood Basalt Province Paul...Roisenberg and D. Stolfa 195 The Karoo Province K. G. Cox 239 Traps of the Siberian Platform V. V...the reviewers formally: they included R. Carlson, K. Cox, A. Dickin, A.J. Erlank, R. Fodor, P. Hooper... Y 28 Wanapum Sh.Cr HAS-40 Pr FSP RS-2 Roza K-9040 HCO-85 54.55 13.33 2.564 13.27 0.256 7.08 2... 47 35 Rough comparisons of basalt volume with K/Ar ages suggest that eruption rate reached a maximum
Report (volume)
Clay (<2 µm) Cation-exchange capacity Extractable K Ch 12: p349, Table 1 entries: 1. Trap Spring oil...for …” p488, l 5, ¶ 2 should read: “… Cs+ > NH4+ ≈ K+ ≈ H+ > Ba+ > Sr2+ ≈ …” Ch 15: p527, l 27: Change... . . . . . . . . ..81 Willhendersonite: Caz(Cao5,K)2[Al6Si6024]·1 OH20 . . . . . ....................... . ...................83 Dachiardite: (Cao 5,Na,K)4[Al4Si20048}18H20 .................... . . . . ........................84 Bellbergite: Ca5(Sr,BaMNa,K)z[Al18Si18072] ·30H20 ............. . .. . .. . .
Book
fallacy. Tectonphysics, 311: 1-29. Tomlison, K. Y., Stevenson, R. K., Hughes, D. J., Hall, R. P., Thurston...Stage, short- CZ6Al, 6°Fe, 36Cl) and long-lived (40 K, 235 U, 238 U and 232Th) radioactive isotopes, produced...materials towards the surface. On Earth, Al, Si, K and Na accumulated as a slag to form the outermost...still abundant; they are 238 U, 235 U, 232Th and 40 K. The rate of heat production from these isotopes (Table...composed of gabbroic anorthosite (predominantly feldspar, lesser pyroxene, with minor garnet, quartz and
 
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