These Videos are really great. Wished you had uploaded them earlier. It would have had helped me so much for my Bachelor. Best regards from a Crystallography master student from Germany 😊
Very inspiring and well explained! I always found difficult to teach these diagrams to students... I use to do that using slides with the different steps. This year I used for the first time the interactive screen (we have in every classroom, but no-one use it) on which you can draw - inspired by your presentation. I feel it was more efficient to explain that way! Cheers from a post-doc from Lausanne, Switzerland!
Sir, thanks for the lecture from Russia. Would you be so kind to make a lecture about really complex ternary diagrams? With phase fields right in the middle of the diagram and complex triangulation. And, at some point, it would be very kind of you to even add some subtitles. Thank you.
My question What is the maximum mass of primary crystals that will form as the batch progress along the cooling path? I though its when t5 is reached at 1300 and the solid mass is 42%. This is the maximum for primary phase right?
Thanks for the helpful explanation. I am studying glaze chemistry for ceramics, and this give me a better understanding of this type of graph. Question if you see it, what determines the starting point in your cooling example for basalt? @5:27
@@kennethbefus gotcha. Temperature is the z-axis and the starting point is whatever molar % of the 3. the starting point and will ultimately determine the % of crystal/solids. It's a bit tricky when it comes to more complex diagrams, but I think I get it. Thanks again.
Very informative indeed! 🙂 I wish all geoscience students had teachers like you.
Thanks a lot for your kind support on this topic. Now I understand it!!
Thanks for the lecture from Brazil!!
These Videos are really great. Wished you had uploaded them earlier. It would have had helped me so much for my Bachelor.
Best regards from a Crystallography master student from Germany 😊
Thank you Sir! You explain everything very well.
Greetings from Germany.
Very inspiring and well explained! I always found difficult to teach these diagrams to students...
I use to do that using slides with the different steps.
This year I used for the first time the interactive screen (we have in every classroom, but no-one use it) on which you can draw - inspired by your presentation. I feel it was more efficient to explain that way!
Cheers from a post-doc from Lausanne, Switzerland!
Thank you for a great explanation. Very helpful!
You may have some interest in a series of videos focused on reading crystallization paths: ruclips.net/video/NuvEzQX0xnk/видео.html
Thanks for the lecture!!
greetings from Israel.
thank you! you're helping confused students on the other side of the world understand this stuff lol
thanks man
It was very helpful
Thank you so muchhh, I can't believe I understand this
Please keep making the videos
Sir, thanks for the lecture from Russia. Would you be so kind to make a lecture about really complex ternary diagrams? With phase fields right in the middle of the diagram and complex triangulation. And, at some point, it would be very kind of you to even add some subtitles. Thank you.
Feel free to check these for more complex diagrams: ruclips.net/video/NuvEzQX0xnk/видео.html
My question What is the maximum mass of primary crystals that will form as the batch progress along the cooling path? I though its when t5 is reached at 1300 and the solid mass is 42%. This is the maximum for primary phase right?
Sir, thank you for the video.love from India. Would you do a video on Thermodynamics part of igneous petrology.
Thank you so much,, I was crying before see this.. now I can do my HW😂💕
Very glad to have helped.
Very well explained, thank you , keep going
Cheers from Indian Institute of Technology (IIT-BHU), India
Thank you for encouragement. Best wishes.
what would happen if temp was around 25 degrees
Thanks for the helpful explanation. I am studying glaze chemistry for ceramics, and this give me a better understanding of this type of graph. Question if you see it, what determines the starting point in your cooling example for basalt? @5:27
Hi. Glad this helped. It was arbitrary starting composition for this example. Any composition would be possible.
@@kennethbefus gotcha. Temperature is the z-axis and the starting point is whatever molar % of the 3. the starting point and will ultimately determine the % of crystal/solids. It's a bit tricky when it comes to more complex diagrams, but I think I get it. Thanks again.
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Professor can I get the name of the text book
The page numbers come from Igneous and Metamorphic Petrology by Myron Best, 2nd edition.
wow, I just finished 2 weeks of class in 26 minutes
🙃
❤❤❤❤❤❤❤. God bless you Sir and answer your prayers in Jesus Name. You have really helped me 😊
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