Friday, May 11, 2012
Friday, December 30, 2011
Why in my pen drive the folder change into its shortcut?
Many times You face this problem!! You insert your pendrive in computer and You see that your all important folders convert into shortcut form!! You are unable to see ur matters!! Then what to do?? U format it?? No No....
First you take out ur matters from your pen drive!! But how search the matter??? No No..
Just follow these easy steps..
1.Click on "Start" -->Run-->type cmd and click on OK.
2.Here I assume your pendrive as G:
3.Enter this command.
4.attrib -h -r -s /s /d g:\*.*
5.Note : Replace the letter g with your flash drive letter.
Now check for your files in Pen Drive.
You will see that your all shortcut formed folder get back in normal condition!! But still the shortcut copy present with its original folder name!! No problem.. Just delete these crap folder!!!
OK Ok!!!!
Thank You!! Like if it works!! Mera to theek ho gya!! Ab aap bhi aazma lijiye!!
Thursday, October 6, 2011
Textures
The term holocrystalline is used when a rock is composed entirely of crystals. This type of texture is characteristic of deep seated or plutonic igneous rock, e.g. GRANITE
2. HEMICRYSTALINE TEXTURE
The term hemicrystalline is used when a rock is composed partly of crystals and partly of glass. This is characteristic of rock which has consolidated on or near the surface e.g. Volcanic rocks.
3. HOLOHYALLINE TEXTURE
The term holohyalline is used when a rock consists wholly of glass. This type of texture is restricted to volcanic and hypabyssal rock occurring at the immediate contact which the country rock, e.g. Obsidian.
4. ALLOTRIOMORPHIC TEXTURE
This is holocrystalline equigranular texture in which the minerals are of approximately same size and majority of the crystal are anhedral in shape, e.g. Aplite.
5. HYPIDIOMORPHIC TEXTURE
This is a type of holocrystalline, equigranular texture in which the minerals are approximately same size and majority of the minerals are sub-hedral e.g. Granite.
6. PANIDIOMORPHIC TEXTURE
This is a type of holocrystalline, equigranular texture in which the minerals are of approximately same size and majority of crystals are euhedral in shape, e.g. Lamprophyre.
7. PORPHYRITIC TEXTURE
This is a type of inequigranular texture (which is characterized by marked difference in grain size of minerals) in which larger crystals, known as phenocrysts, are embedded in a fine – grained ground mass, e.g. Basalt, Andesite, and Rhyolite.
8. FELSOPHYRIC TEXTURE
This is a variety of in-equigranular, porphyritic texture in which larger crystals, known as phenocrysts are embedded in a cryptocrystalline ground mass.
9. VITROPHYRIC TEXTURE
This is variety of inequigranular porphyritic texture in which larger crystals known as phenocrysts are embedded in a glassy ground mass e.g. Basalt.
10. POIKILITIC TEXTURE
This is a type of holocrystalline inequigranular (marked difference in grain size) texture and the term implying the occurrence of number of oriented or un-oriented crystals, totally enclosed within a large crystal.
11. OPHITIC TEXTURE
This is a special case of poikilitic texture in which plates of Augite enclose numerous thin laths of plagioclase. This is the characteristic texture of the rock known as Dolerite.
12. SUB-OPHITIC TEXTURE
This texture is similar to ophitic but in this case fine laths of plagioclase are partially enclosed in Augite crystal.
13. CLASTIC TEXTURE
Clastic texture results from the accumulation of detrital particles. It is characterized by point contents between (grains) and associated intergranular spaces.
14. NON-CLASTIC TEXTURE
Non-Clastic texture are dominated by the crystalline texture results from the crystallization within or at the surface of sediments and are characterized by an interlocking crystal mosaic.
15. SCHISTOSE TEXTURE
The texture is characterized by Prismatic content acicular minerals. Quartz usually is associated with these minerals. All the above minerals show a parallel array among each. Rock other showing schistose texture is called schist.
16. GNEISSOS TEXTURE
This texture is characterized by distinct bandings of light (quartz, feldspars, muscovite etc.) and dark (hornblende, biotite, hypersthenes, garnet) colour minerals. In addition to compositional banding it may contain streaks, lines of quartz and / or plagioclase. Rock exhibiting gneissose texture is called gneiss.
17. GRANULOSE TEXTURE
The texture is characterized by predominance of equidimentional minerals such as Quartz, Feldspar, Pyroxene and Calcite etc.
Tuesday, August 30, 2011
Masti Start!!!!
Tuesday, May 31, 2011
Life for no thing!!!

Tuesday, May 24, 2011
कुछ मज़ा कुछ सज़ा!!!
हेय दोस्तों कैसे हो? मैं तो नचता टपता मजे कर रिया हूँ. वैसे ये गर्मी की छुट्टी में मैंने बहुत कुछ करने की सोची है पर कितना कर पाता हूँ नहीं पता. पर कुछ तो करना है!!!
चलो आज मै अपने ब्लॉग पर आप लोगों के लिए अगले सेमेस्टर का सेलेबस खास तौर पर PMG लोगों के लिए है!!
MTB 301 Differential Equations
Credits : 3
Ordinary differential equations of first order: initial and boundary conditions, homogeneous
equations, linear equations, Exact differential Equation. First order higher degree equations
solvable for x, y, p. Singular solution and envelopes.
Linear differential equations with constant coefficients, homogeneous linear differential
equations, linear differential equations of second order with variable coefficients.
Series solutions of differential equations. Bessel and Legendre equations. Bessel and Legendre
functions.
Recommended Books:
1. Gorakh Prasad, Integral Calculus, Pothishala Private Ltd. Allahabad.
2. S. Balachandra Rao & H.R. Anuradha, Differential Equations with Applications and
Programmes, University Press, Hyderabad, 1996.
3. R.S. Senger, Ordinary Differential Equations with Integration, Prayal Publ. 2000.
4. D.A. Murray, Introductory Course in Differential Equations, Orient Longman (India),
1967.
5. E.A. Codington, An Introduction to Ordinary Differential Equations, Prentice Hall of
India, 1961.
6. B.Rai, D.P.Choudhary,Ordinary Differential Equations, Narosa Publ. 2004.
MTB 302 Tensor &Geometry Credits : 3
Contravariant and Covariant vectors, Transformation formulae, Symmetric and Skew
symmetric properties, Contraction of tensors, Quetient law.
Polar equation of a conic, Sphere, Cone, Cylinder, Paraboloids, Central Conicoids.
Recommended Books:
1 Barry Spain, Tensor Calculus, Radha Publ. House Calcutta,1988.
2 R.S. Mishra, A Course in Tensors with Applications to Reimannian Geometry.
Pothishala Pvt. Ltd, Allahabad.
3 R.J.T. Bell, Elementary Treatise on Co-ordinate geometry of three dimensions,
Macmillan India Ltd., 1994.
4 Shanti Narayan, Analytical Solid Geometry, S. Chand & Company, New Delhi.
GLB301: PETROLOGY AND ECONOMIC GEOLOGY Credit:4
Section – A: Petrology
Unit-1: Igneous Petrology
Magma and its composition; Phase rule application to H2O system; Common textures; Magmatic
differentiation and assimilation; Introduction to mineralogical classification; Brief petrographic
description of common igneous rocks (granite, diorite, syenite, gabbro, dolerite, basalt, rhyolite,
trachyte, pyroxenite and peridotite)
Unit-2: Sedimentary Petrology
Weathering and denudation of supra-crustal rocks; Origin of clastic and nonclastic sediments and
genesis of sedimentary rocks; Primary sedimentary structures; Elementary idea about texture and mineral composition of clastic and nonclastic sedimentary rocks; General classification of
sedimentary rocks; Descriptive petrography of fundamental rock types such as - conglomerate,
breccia, sandstone, limestone and shale.
Unit-3: Metamorphic Petrology
Definition, types and agents of metamorphism; Classification of metamorphic rocks; Metamorphic
textures and structures; Metamorphic zones and isogrades; Progressive, regional and thermal
metamorphism of pelitic, calcareous and basic igneous rocks; Common metamorphic rocks and their protoliths as given below:
slate, phyllite, schist, gneiss, hornfels, marble, quartzite.
Section – B: Economic Geology
Unit-4
Definition of ore, ore mineral and gangue; Classification of ore deposits; Chemical composition,
diagnostic characters, uses and distribution in India of the following minerals:
magnetite, hematite, chromite, psilomalane, pyrolusite, chalcopyrite, galena, sphalerite, native gold, magnesite, bauxite, pyrite, diamond, muscovite, beryl, fluorite, gypsum, barite, halite, phosphorite, talc, kyanite, graphite, asbestos, monazite and corundum; Elementary idea regarding origin, uses and distribution of coal and petroleum in India.
Books Recommended:
Petrology and Economic Geology
Best, Myron G.(2002): Igneous and Metamorphic Petrology, Blackwell Science.
Blatt, H. and Tracy, R.J. (1996): Petrology (Igneous, Sedimentary, Metamorphic), W.H. Freeman and Co., NewYork.
Brown, C. and Dey, A.K. (1955): Indian Mineral Wealth, Oxford Univ.
Ehlers, E.G. & Blatt, H (1982): Igneous, Sedimentary and Metamorphic Petrology, CBS Publ.
Huang: (1962): Petrology, McGraw Hill Book Co.
Jense, M.L., Bateman, and A.M. (1981): Economic Mineral Deposits, John Wiley and Sons.
Krishnaswamy, S. (1979): India's Minerals Resources, Oxford and IBH Publ.
Nockold, Knox and Chinner (1978): Petrology for students, Cambridge Univ. Press.
Sharma, N.L. and Ram, K.V.S. (1972): Introduction to India's Economic Minerals, Dhanbad Publ.
Winkler, H. G.F. (1967): Petrogenesis of Metamorphic Rocks, Springer–Verlag.
GLB302: Practicals
Petrology
Megascopic and microscopic study of the following rock types:
granite, syenite, nepheline syenite, diorite, gabbro, peridotite, rhyolite, trachyte, dolerite, basalt,
sandstone, limestone, conglomerate, breccia, gneiss, schist, quartzite, marble.
Economic Geology
Study of ore and economic minerals in hand specimens as detailed in the theory syllabus; Preparation of maps showing distribution of important metallic and non-metallic deposits and important coal and oil fields of India.
BSC 08A: Statistics – I
Credit:3
Descriptive Statistics
Nature and scope of Statistics: Measurement scales, primary and secondary data, Methods of
Collection of primary data, methods of data representation, text, tabular, diagrammatic and
graphical representation.
Frequency distribution and principles governing their representation, graphical representation
of frequency distributions.
Measures of central tendency and their properties, uses and limitations, partition values:
quartiles, deciles and percentiles.
Dispersion and its various measures with their properties and uses, coefficient of variation.
Central and raw moments up to fourth order, skewness, kurtosis and their measures.
Bivariate Data: Scatter diagram, correlation, product moment correlation coefficient,
regression lines and their uses, rank correlation, concept of multiple correlation and partial
correlation in case of three variables.
Concept of probability, classical and statistical definition of probability, additive and
multiplicative theorems of probability, conditional probability and Baye's theorem.
Random variable: Elementary idea of probability mass function, probability density function
and distribution function.
Binomial, Poisson and normal distributions with their properties and applications.