ODH019: Magmatic-hydrothermal systems and the formation of epithermal deposits - Jeffrey Hedenquist

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Ore Deposits Hub

Ore Deposits Hub

Күн бұрын

Пікірлер: 32
@SEGbetaTest
@SEGbetaTest 4 жыл бұрын
Hmm, at least one to date is not a happy camper over the talk. Perhaps I did not give enough hints on where the next discovery will be (or rather, is). Thanks to the rest for watching. As the Ore Hub organizers said, slides are available at Research Gate.
@TheJoseph0012
@TheJoseph0012 3 жыл бұрын
Where will the next discovery be? 😏
@igotufoinformation9636
@igotufoinformation9636 2 жыл бұрын
😄
@pelletierjocelyn5564
@pelletierjocelyn5564 4 жыл бұрын
Jeffrey Hedenquist is from far the most qualified geologist that studied the Epithermal deposits. Thanks for his great generosity and to team that organized this great ''event''.
@robertmoye7565
@robertmoye7565 Жыл бұрын
Excellent presentation with great information backed by real world examples.
@rodneyjsnider8540
@rodneyjsnider8540 2 жыл бұрын
Bravo, nice description of the magmatic systems!
@christianenriquevargassern2620
@christianenriquevargassern2620 4 жыл бұрын
Merci beaucoup, grand présentation!
@abdonecbishop
@abdonecbishop 2 жыл бұрын
Enjoyed....nice video........ in the cartoon at 8:17:07...... May we imagine putting a physic's Hamiltonian operators for (Uranium, K) nuclei concentration at base of porphyry outlined in cartoon. That will simulate/generate a broad smooth vertical temperature gradient up and into the surrounding lithosphere or cap rock containing an epidote-chlorite solid-solution major mineral embedded in whole rock major mineral assemblage and used to classify the type of rock observed.
@abdonecbishop
@abdonecbishop 2 жыл бұрын
The cartoon's vertical scale is important, where would the Moho be placed relative to the base of porphyry, assuming the porphyry is a cooled residual magma chamber that once in the past had a much lower viscosity than its surrounding lithosphere. The magma chamber viscosity models to be dependent on the proportions of crystal to fluid bound by the walls of the magma chamber. Work is done by both conductive and convective forces acting in the magma chamber, exerting a differential pressure and temperature across a solvus surface that is the boundary of the magma chamber. The magma chamber can be characterized as a 3-cycle Carnot motor doing work on upper lithosphere, fueled by the free energy released through weak force K and U decay events, generating both local density and temperature changes within the magma chamber.
@meilani-2163
@meilani-2163 2 жыл бұрын
Thankyou Pak Jeffrey!
@nurhadiwibowo3978
@nurhadiwibowo3978 4 жыл бұрын
Good presentation and recharge the exploration energy
@diegofebrerovalenzuela6348
@diegofebrerovalenzuela6348 3 жыл бұрын
22:36 That is the fluid that carry the most of the ore? also metals in that fluid are in liquid or gas state?
@ahmedaldom7150
@ahmedaldom7150 2 жыл бұрын
Thank you so much for information ☺
@anagy20
@anagy20 8 ай бұрын
9:55 omg Universidad de Bogotá. MI GENTE LATINO. Psa: Thanks for the presentation.
@goodman1098
@goodman1098 4 жыл бұрын
Nice presentation, a huge thanks 😊
@antonkutyrev3090
@antonkutyrev3090 4 жыл бұрын
Very useful lection, thank you!
@kyihtun7491
@kyihtun7491 4 жыл бұрын
Thank you for excllent presentation
@simabayat2175
@simabayat2175 4 жыл бұрын
great presentation, thanks
@andrewt5400
@andrewt5400 4 жыл бұрын
how about obout southern Chile below 600m ...near coast?
@edward05lan
@edward05lan 3 жыл бұрын
Thanks for sharing
@6554532
@6554532 4 жыл бұрын
Great presentation! What is the typical depth base of HS environment to porphyry? 1-2km? Yanacocha has some classic transitional features like patchy and wormy texture. But I wonder if the porphyry below is too deep to be economic? The Lepanto example seems different from the classic model in which the lithocap sits off the the side porphyry center.
@SEGbetaTest
@SEGbetaTest 4 жыл бұрын
The transition is typically ~1 km below the paleosurface. The Lepanto lithocap and enargite-Au deposit, offset from the deeper Far Southeast porphyry, is typical of this relationship. The epithermal environment at
@indonesiangeologist5993
@indonesiangeologist5993 4 жыл бұрын
Many thanks !!
@melissarodriguez9757
@melissarodriguez9757 4 жыл бұрын
Merci beaucoup!
@6554532
@6554532 4 жыл бұрын
Please upload Antonio's Nov 25th talk on AA alteration
@SEGbetaTest
@SEGbetaTest 4 жыл бұрын
All Ore Hub talks are on YouTuba a day or two after presentation. Antonio's talk on advanced argillic alteration is at: kzbin.info/www/bejne/hZTRgGitfbWgm7s Also a talk on the same subject, in Spanish , at: kzbin.info/www/bejne/Z5DdkKqIiLmooas
@valls_geoconsultant
@valls_geoconsultant 4 жыл бұрын
the slides are not showing
@jeanpazhuaman7410
@jeanpazhuaman7410 4 жыл бұрын
Thanks a lot!
@junioralejandro1071
@junioralejandro1071 4 жыл бұрын
Pasen las diapositivas
@RustyAtwood-s1p
@RustyAtwood-s1p Ай бұрын
Thanks for the info in this video ☺️ Owner of Alaska Rare Earth LLC
@cooljingmoney
@cooljingmoney 4 жыл бұрын
thanks!
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