วีดีโอ

do you always align the strike to the north pole?

Nice introduction 👍

Why did the graph start at 350 million years ago? Or in other words, how do you go about determining where a certain sample should start on a specific time scale when this dating technique is suppose to determine how old said sample is? Or am I completely missing something?

In several texts they claim that subduction happens because oceanic crust is more dense than continental crust but that doesn't make any sense yes it is dense but it was still floating over the mantle . So what actually happened at the collision that it got subducted and not before it?

i have a question how could differenciate in parallel extiction and undulose extiontion bcz one represents that the mineral undergoes deformation while the other just give is the knowlage that the minerla which we are examine is biotite mica

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Sorry, I'm probably missing something, but is the dotted line respresentive of the Nd144 content in the samples?

Doesn't Nd-144 decay as well? Wouldn't you want the isotope in the denominator to be a stable isotope?

4:27 so only during this crystallization process can these different minerals absorb the Samarium parent atom? They can't absorb it before crystallization or afterward?

Damn we got thin section 2 before gta 6

8:20 was groundbreaking for my learning, wish I saw this earlier.

How can we distinguish pyroxene if the cleavage isn't clear ? I'm finding it hard to recognize the interference colors orders

Nice demonstration

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I didn't understand the purpose of this diagram. This is what GPT4 says: This is a description of how to plot the orientation of a geological plane (like a bedding or fault plane) on a stereonet, which is a tool used by geologists to visualize and analyze the orientation of planes and lines in three dimensions. In essence, by following these steps, you are able to visualize the orientation of a geological plane on a two-dimensional surface. This process helps geologists in understanding structural relationships in rock bodies, which can be crucial for various purposes like understanding tectonic histories or planning in engineering geology.

The cement of the sample are Fe oxides?

good vid, thanks a lot

Thank you

Really appreciable work.

It takes a lot of balls to perform this experiment.

i love that thanks

Wonderful!

Excellent video. Thank you so much!

Send me dm on messenger.thanks.. i want to know about my rocks.. i found this, with his broken parts.. this is beautifull rocks with a shinny small crystal

I have that looks like in my rocks.. please dm me for the picture sample of my rocks.. please help me. I send you a picture of my bluish green rocks...

great work

Please upload more metamorphic rocks thin section videos.

So well explained, totally understood now. Thank you so much!

cool

very informative, thanks so much

This is very useful 👍👍 Thanks ☺️

Thank you such easiest and awesome interpretation . waiting for more contents

Thank you for the video. It would be very, very informative to show, with arrows, where side is north, directions of the flows/cross beding, and the mouth of the delta.

This thinsection has no microcline, this grain and others are products of silisification of dolomite, you can sea rhomboid shape of grains, its result of my unpublished work and this type of silisification has several by product and can create diagentic sandstones, you can use staning method, you will sea surprisingly, it is not a microcline grain

answer should be 25°/332°

he went into the freezing ocean for this. jeez my man

Wonderful keep uploading more

Pretty

Thank u so much🙏🏽

Thank you 🌹

please create more videos on petrography and if possible on petrogensis too

this was so clear! thank you so much :)

Thank you very much .

you only showed 4 balls!

Thanks!

ive learned more in 5 minutes, than i have in 7 hours of class today. thank you very much

You just got rock rolled

Lam-mince

HI