Igneous Petrology Series: Lesson 9 - Ternary Peritectic Phase Diagrams

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Welcome to the Igneous Petrology Series.

The igneous petrology series is a series of short and simple educational videos on topics such as thermodynamics, geochemistry, and geology.

In the fundamentals playlist, I talk about thermodynamics, element classification, and phase diagrams. These can be quite complicated subjects, but once they're broken down, you'll see they are not quite as daunting as first thought!
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I think this is the best explanation of ternary peritectic....Good work really appreciate

TrendsinGeology
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Great video! I have a question about the green point which dodges the peritectic point at 5:03. Does that mean in the end when the entire liquid is cooled that there is a mineral assamblegde of forsterite (Olivin), enstatite, anorthite and cristobalite? Because by doging/bypassing the peritectic point the olivin does not get the chance to break down by reacting with the melt and form more enstatie?

mastermuffin
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How do you project your own experimental liquids on this projections? Any useful softwares?

weronikaofierska
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Let's add a point here. The An-En join will not intersect the peritectic reaction curve. If intersect it will not a peritectic curve rather we can call it as a cotectic curve like other cotectic curves.

aumprkashsahoo
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merci pour cette vidéo c'est une vraie mine d'or (un peu comme celles dans le Yukon chez vous les américains(piou piou))

dodo_drone
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Thanks for really helpful videos.
I have a question! Do the track of ternary diagrams have any differences between equilibrium and fractional crystallization?

bonakim
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Plzz make vid for diopside forsterite silica ternary system. plzzz

suchitraagrahari
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Why do we draw a line from the enstatite end member tbrough the system? Why do it dodging the peritectic point?

farihatasnim