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Splendid way of illustration
Excellent!🤩, keep it up 👍
Thank you 😊
Sir please explain about sedimatory environment and facies
Excellent teaching..tq
What could be the possible path for magmatic underplating in normal thickened crust? is it a retrogressive path?
regional and thermal metamorphism of parent rocks?
Perfect
So well explained 😃
Nice sir 🙏🙏🙏
Nice explaining
Metamorphic reactions ki video chahiye
In third case how there is sudden cooling after magmatic heating
because there isn't any magmatic chamber but atonce there come magma and by this rapid increase and cooling of temperature
Describe stability limits of various rocks and minerals as a function of p and t in the metamorphism?is it's answer is pT path sir?
Stability fields are for minerals like spinel, garnet ertc. Depending on the varying temperature pressure conditions with depths within crust
Sir if we are asked to discuss about domain of metamorphic facies using PT diagram,can we write this answer as explained by u?
Watch my video on metamorphic facies, relate both the videos and write the answer
In anticlockwise loop what is the condition of pressure increase please give an example
Please Watch the video after 26.20 min
Tnk u sir🙏🙏👍👍
When Graph is showing P and T only why it is P,T and t graph
t is for time!
Yes sir you have mentioned that in video..but my Q. is time is not mentioned in graph
But it's alright..I should not mull over these tiny things .Thank you for such a quick responseYour way of teaching is really nice. Keep it up. I really got inspired by ur videos.
Thank you 😇😇
Splendid way of illustration
Excellent!🤩, keep it up 👍
Thank you 😊
Sir please explain about sedimatory environment and facies
Excellent teaching..tq
What could be the possible path for magmatic underplating in normal thickened crust? is it a retrogressive path?
regional and thermal metamorphism of parent rocks?
Perfect
So well explained 😃
Nice sir 🙏🙏🙏
Nice explaining
Metamorphic reactions ki video chahiye
In third case how there is sudden cooling after magmatic heating
because there isn't any magmatic chamber but atonce there come magma and by this rapid increase and cooling of temperature
Describe stability limits of various rocks and minerals as a function of p and t in the metamorphism?is it's answer is pT path sir?
Stability fields are for minerals like spinel, garnet ertc. Depending on the varying temperature pressure conditions with depths within crust
Sir if we are asked to discuss about domain of metamorphic facies using PT diagram,can we write this answer as explained by u?
Watch my video on metamorphic facies, relate both the videos and write the answer
In anticlockwise loop what is the condition of pressure increase please give an example
Please Watch the video after 26.20 min
Thank you 😊
Tnk u sir🙏🙏👍👍
When Graph is showing P and T only why it is P,T and t graph
t is for time!
Yes sir you have mentioned that in video..but my Q. is time is not mentioned in graph
But it's alright..I should not mull over these tiny things .
Thank you for such a quick response
Your way of teaching is really nice. Keep it up. I really got inspired by ur videos.
Thank you 😇😇