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Dr Vikram Pratap Singh
India
Приєднався 10 жов 2009
Associate Professor, Geology, IGNTU Amarkantak
PhD from DU
MSc Geology from BHU
BSc (Hons) Geology from BHU
PhD from DU
MSc Geology from BHU
BSc (Hons) Geology from BHU
SUPERCONTINENTS IN EARTH'S HISTORY
Lecture on the formation of various landmasses in the Earth's history
Переглядів: 159
Відео
Type Specimens in Paleontology
Переглядів 11514 днів тому
It is an important lecture that will help in GSI and other competitive exams.
Why is seawater neutral when the total concentration of anions is more than cations?
Переглядів 1542 місяці тому
Illustration of Law of Constant Proportions and Charge balance in seawater.
Effect of Diagenesis on Sandstone Reservoir
Переглядів 1,9 тис.3 роки тому
Effect of Diagenesis on Sandstone Reservoir
Petroleum Reservoir Rock Characteristics
Переглядів 3,3 тис.3 роки тому
Petroleum Reservoir Rock Characteristics
Petroleum Source Rock and Generation of Petroleum
Переглядів 10 тис.3 роки тому
Petroleum Source Rock and Generation of Petroleum
Physical Description of Coal- Lithotypes
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Physical Description of Coal- Lithotypes
Conditions for development of coal seams- Part 2
Переглядів 7203 роки тому
Conditions for development of coal seams- Part 2
Conditions for development of coal seams- Part 1
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Conditions for development of coal seams- Part 1
Geological Basis of Coal Formation- Importance of Climate, and Paleogeography
Переглядів 1,3 тис.3 роки тому
Geological Basis of Coal Formation- Importance of Climate, and Paleogeography
Geological Basis of Formation of Coal- Evolution of Flora
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Geological Basis of Formation of Coal- Evolution of Flora
Deccan Volcanic Province (Western Deccan Plateau)
Переглядів 2,3 тис.3 роки тому
Deccan Volcanic Province (Western Deccan Plateau)
Sir was there no life before proterozoic? I thought stromatolites were present during archean
Yes there are evidences of life during Archean and Proterozoic. Those algal mats got fossilised which we call as stromatolites today. But the complex forms or in true sense, the life started during Edicaran (Neoproterozoic).
Thank you Sir for this video😊 Please make video on Geodynamics
18:04 sir if during proterozoic there was active tectonism then how does it promote crustal stability?
It’s a good question. The crustal stability means the formation of a shield, which has both stable craton and tectonically formed mobile belt. When both are formed, the landmass becomes stable on which further processes of erosion and deposition occurs.
@@MrVikramsingh1Understood sir. Thank you
Equatorial easterly winds are also known as Trade winds
Thank you sir Kindly make more video on ore geology please sir
Please make video on petrolgy
Thank you so much sir
Please upload triclinic system
The sound in the initial part of this video is not clear, but it is not important stuff. The remaining part where calculation is explained, there the voice is clear. Still if anything isn't clear, please drop a message.
Sir please discussion about last 3 years CSIR NET papers sir.
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1000% Best Lecture of Singhbhum supergroup ,Sir u covered all the things in a great way; Thank u so much for this fruitful session.
Excellent lecture sir. Very well explained in a lucid manner
Sir,please upload videos of EGMB & SGT also
Sir any Paid courses for more subjects?
@@Ranjeet_Mahto01 I didn’t get you!!
Sir please can i get you email id
Sir hindi me bhi bol kar samjha dijiye
Sir plz hindi me bhi पढ़ा दीजिये
अलग से वीडियो बनाना मुश्किल है। आप गूगल मीट पर मुझसे हिन्दी में समझ सकते हैं। जब भी करना हो एक मेल भेज दीजिए
Try to cover other dimensions of geology too sir thankyou very much for your kind efforts 😊please keep up the good work 🙏
Tanks sir 🙏🏻 Sir kya aap इसे hindi me bol kar samajha sakenge आपकी bahut kripa hogi
@@anupamasingh6541 बिलकुल समझा देंगे लेकिन वीडियो पे नहीं, आपको एक ऑडियो नोट्स बना कर भेज देंगे। आप अपना ईमेल भेज दीजिए
thank you for your very nice description
Thankyou
Thank you so much 😊 sir
Sir a question in which mentioning about increasing order of depth of deposition.. Pteropod ooze is made up of aragonite composition, then it will have to come before lepidocyclina limestone bcz aragonite as compared to calcite have less stability. Then why it comes after lepidocycljna limestone instead of its composition is aragonite.
If you listen to the explanation of that questions carefully, you will get the answer. It’s not just the composition but the depth at which a certain organism lives. Except the Lepidocyclina, all others are planktons. It means all the other three live in open ocean while Lepidocyclina lives in shallower depths. So its tests will be deposited at shallower depth. That is why its ooze is shallowest. The other three which live in open ocean will be deposited as per the lysocline.
@@MrVikramsingh1thankyou sir...
Equatorial easterlies also called.... Trade wind
Appreciable content and thank you sir
Sir I have a doubt related to fluvial and glacial environment facies in sedimentary
@onlyfact1115 go ahead and send it
How Anastomosing have several major channel and what process are responsible for making Anastomosing in fluvial
@onlyfact1115 Anastomosing river channels form through a combination of processes: Tectonic stability: Low tectonic activity allows rivers to maintain a stable course over time. High sediment load: Rivers carrying high amounts of sediment, especially fine-grained particles, deposit material along their banks, creating multiple channels. Aggradation: Sediment deposition raises the riverbed, causing the river to overflow and create new channels. Avulsion: Sudden changes in the river course, often due to flooding or sediment blockages, lead to the formation of new channels. Meandering: Rivers with high sinuosity can develop multiple channels as meanders are cut off or abandoned. Wetland or floodplain interaction: Rivers flowing through wetlands or floodplains can create multiple channels due to interactions with soft sediments and vegetation.
Thank you sir for giving your valuable time and I will note down in my notes, now
thank you for the explanation in english
Nobody could have taught this in such manner that too diagrammatically. Thank you very much sir!!!! you really made it simple and easy understand, looking forward to more video of yours in geology in such way. Thank you once again.
Namaskar sir please sir continue this series with recent csir net questions papers.
Namaskar sir this is much helpful series sir if possible continue this series sir
Namaskar sir thanks sir it much helps in preparation and clear my much doubt.
Please sir continue this series. It really much helps in preparation for NET.
Wrong explanation of traps.... Trap is derived from Swedish word trappa meaning step like hill...
Thanks
Thanks a lot sir ❤ . recent csir net ki questions papers discussion hoseketo bahat madat hojata sir
Thank you sir for this amazing video because I was waiting from long times
Hlo sir I have a question please do reply it in detail.sir do rectify me if I am wrong .as of my understanding I think TTG are formed at convergent plate boundaries but that too only when the one plate is is continental in nature .and also TTG are formed at divergent plate boundaries but only when the divergence takes places between two continental plates.is it right?
Currently I am in Germany and will reply to you in detail once I get back. Send me your email.
Great explanation, sir
Hii sir ...which book you have used?
Petroleum geology by RC Selley and Another book by Levorsen
Pdf sir
Send me a mail
Amazing explanation sir
Sir! 1. What should be do before preparation of net exam . 2. Is syllabus sufficient for cracking this exam
Yes, definitely
Amazing explanation sir. Please provide cudappah , vindhyan basin video if possible
Very good and best explanation sir
Thanks a lot for this Sir
Thankyou professor. Much appreciated explanation
Sir It's Very helpful and anyone can easily understand
Sir olz recity me if I'm wring when two plates shows convergent movement and both plates are oceanic as a result of that conversion island arc will form is it? But you told in case of oceanic convergent movement volcanic arc will form .upto up understanding volcanic arc form when convergent movement is between oceanic olaye and continental plate plz answer?
Island arc is formed due to convergent motion of continental plate and oceanic plate.
Sir pls can you give me a link to your slides
I haven’t uploaded these slides anywhere.
oh such a nice and valuable piece,i like the detailed and and easily understood explanation you give