Awesome presentation Geo girl, I am happy that we are getting to learn from someone from another Continent and best thing about that is learning different things because we use different textbooks. I had not learned about P-TCO2 transition previously, happy that you discussed and thanks for the links too.
Of course! So glad you found it helpful! Actually I didn't even get the P-T-CO2 graphs from my textbook, I got them from the Alex Strekeisen website, it is such a great resource! Honesetly, I wish I had found these resources when I was taking this class haha!
Another very fascinating video as expected. You’re outstanding videos never disappoint because you always make the best content which is one of the reasons why it’s always such a tremendous pleasure for me to learn with you my favorite teacher. You’re so beautifully gifted and intelligent my friend. You’re the best. 😊❤😉👍
@@GEOGIRL You’re very welcome my friend. 👍 You’ll always have my full support and encouragement. 😉 I hope you have a wonderful day as well. 😊 You’re absolutely amazing Rachel. ❤️
I think it’s great how you use the proper terms. Have you done just metamorphic facies yet? We still have this problem in geology where one guy’s sandstone is another’s quartzite. Especially in the zeolite and lower greenschist facies.
Well my first video on metamorphic petrology was kind of an overview and I talked about the line between diagenesis and metamorphism as well as the other end of the spectrum with the line between metamorphism and melting. But I haven't done a video all about facies, that is a great idea, thanks! ;)
very cool subject GEO GIRL . Can we actually make these rocks? sounds like we know how they we're made. pressures, heat, electricity, what else do you need? pretty sure Ancient builders did it regularly.
To my understanding skarns are calc-silicates. But in general I have noticed that samples defined as skarn seem to be more rich in Mg, Fe, Mn, & Al silicates and just overall 'dirtier' than when I samples defined as calc-silicate, so my guess is skarns are just on the more detrital/silicate-rich end of the calc-silicate scale. Hope that helps ;)
@@manishajindal85 Oh cool I didn't know that, thanks for sharing! Well like I mentioned in the video, the silicates in calc-silicates are mostly detrital in origin (to my understanding) which means they they form in a sedimentary environment, potentially a carbonate platform with a lot of river input from a delta (where the carbonate platform promotes carbonate formation, while the river input adds the detrital silicates). Then after burial, this impure carbonate rock gets metamorphosed into a calc-silicate. Hope that helps ;)
Awesome presentation Geo girl, I am happy that we are getting to learn from someone from another Continent and best thing about that is learning different things because we use different textbooks. I had not learned about P-TCO2 transition previously, happy that you discussed and thanks for the links too.
Of course! So glad you found it helpful! Actually I didn't even get the P-T-CO2 graphs from my textbook, I got them from the Alex Strekeisen website, it is such a great resource! Honesetly, I wish I had found these resources when I was taking this class haha!
I think I’ll watch this one for educational purposes not entertainment.
I ❤️ GEO GIRL
THANK you so much. you really have helped me better understand my Geology classes.
Thanks for the comment! I am so glad to hear that! ;D
Its so cool that Gal Gadot opted geology in her college, btw very much helpful lectures.. Thanks
This is my fav comment ever, thank you! ;)
TY this helps me understand metamorphism better.
So glad you found it helpful ;D
Nice presentation
Another very fascinating video as expected. You’re outstanding videos never disappoint because you always make the best content which is one of the reasons why it’s always such a tremendous pleasure for me to learn with you my favorite teacher. You’re so beautifully gifted and intelligent my friend. You’re the best. 😊❤😉👍
Thank you !! You are also the best for being so supportive and encouraging! ;D
@@GEOGIRL You’re very welcome my friend. 👍 You’ll always have my full support and encouragement. 😉 I hope you have a wonderful day as well. 😊 You’re absolutely amazing Rachel. ❤️
I think it’s great how you use the proper terms.
Have you done just metamorphic facies yet? We still have this problem in geology where one guy’s sandstone is another’s quartzite. Especially in the zeolite and lower greenschist facies.
Well my first video on metamorphic petrology was kind of an overview and I talked about the line between diagenesis and metamorphism as well as the other end of the spectrum with the line between metamorphism and melting.
But I haven't done a video all about facies, that is a great idea, thanks! ;)
@@GEOGIRL I must go look at that video. I don’t remember it. Keep on doing good work
@@stevenbaumann8692 Thanks Steve! And right back at you ;)
Very nice explanation..🙃🙃
Thank you ;D
@@GEOGIRL most welcome..🙃🙃🙂
awesome!
very cool subject GEO GIRL . Can we actually make these rocks?
sounds like we know how they we're made.
pressures, heat, electricity, what else do you need? pretty sure Ancient builders did it regularly.
Absolutely we can! :D
Love from INDIA :^)
Impressive 👍😁
Thank you! ;D
i need more information of magnesite mgco3 which coming from serpentinite rocks
Thanks for the comment, I will look into it and see what I can do ;D
Awesome explanation🥰. plz send your Geochemistry video link mam
Thank you! And I am sorry, but which geochem video are you refering to? Did I refer to something and forget to link it?
Thanks!
How to differentiate between a calc-silicate rock and a skarn?
To my understanding skarns are calc-silicates. But in general I have noticed that samples defined as skarn seem to be more rich in Mg, Fe, Mn, & Al silicates and just overall 'dirtier' than when I samples defined as calc-silicate, so my guess is skarns are just on the more detrital/silicate-rich end of the calc-silicate scale.
Hope that helps ;)
Skarns are formed when there is igneous intrusion into the carbonate rocks. Can you please shed some light on the origin of calc-silicate rocks?
@@manishajindal85 Oh cool I didn't know that, thanks for sharing! Well like I mentioned in the video, the silicates in calc-silicates are mostly detrital in origin (to my understanding) which means they they form in a sedimentary environment, potentially a carbonate platform with a lot of river input from a delta (where the carbonate platform promotes carbonate formation, while the river input adds the detrital silicates). Then after burial, this impure carbonate rock gets metamorphosed into a calc-silicate.
Hope that helps ;)
Plate tectonics of middle earth. How's the archenstone formed
Is this a video request? I am not sure what archenstone is? Can you enlighten me? haha
You don't know your Tolkien? The hobbit. It belongs to thorin oakenshield
@@TheChuckwagonLite Oh my bad! I don't remember that haha
Hello geo girl
Looking so beautiful..🙃🙃
How are you
I am doing great! And you? How are you liking the video? ;)
Today I am the first who's like and comment
Almost every single time it's you, you are so fast! haha
Hii..geo girl...