Natasha (@mantlerocks) 's Twitter Profile
Natasha

@mantlerocks

Geologist & Research Scientist @UBCeoas. Mantle xenoliths, igneous petrology, geochemistry, isotopes, critical minerals, etc. #NatGeo Explorer '20. she/her

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calendar_today17-09-2011 04:08:57

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Natasha (@mantlerocks) 's Twitter Profile Photo

Think I got the coolest birthday present ever! 😍☄️ #pallasite #meteorite #teamolivine #outofthisworld #thinsectionmaybe?

Think I got the coolest birthday present ever! 😍☄️ #pallasite #meteorite #teamolivine #outofthisworld #thinsectionmaybe?
University of Alberta SEG Student Chapter (@uofa_seg) 's Twitter Profile Photo

Our SEG Student Chapter is extremely thankful for all the support and mentorship Roger Morton has given our economic geology students. If you'd like to attend his Celebration of Life, please see the info in the link - UofA SEG student executive committee. edmontonjournal.remembering.ca/obituary/roger…

Natasha (@mantlerocks) 's Twitter Profile Photo

Fancy a whisky drink with some Acasta “gneiss” cubes? ⛏🥃#oldestwhiskystones #geologylife #writingmythesisnow...

Fancy a whisky drink with some Acasta “gneiss” cubes? ⛏🥃#oldestwhiskystones #geologylife #writingmythesisnow...
Natasha (@mantlerocks) 's Twitter Profile Photo

Successful mineral auction this year. All those hours making coasters and whisky ice cubes paid off... #mineralcollectors #geologistlife

Successful mineral auction this year. All those hours making coasters and whisky ice cubes paid off...
#mineralcollectors #geologistlife
Natasha (@mantlerocks) 's Twitter Profile Photo

My contribution to #ThinSectionThursday shows garnet rims forming between clinopyroxene and plagioclase, while garnet is also breaking down to spinel. Orthopyroxene (containing garnet exsolution) is also surrounded by this corona of clinopyroxene and garnet. Lots going on!

My contribution to #ThinSectionThursday shows garnet rims forming between clinopyroxene and plagioclase, while garnet is also breaking down to spinel. Orthopyroxene (containing garnet exsolution) is also surrounded by this corona of clinopyroxene and garnet. Lots going on!
Natasha (@mantlerocks) 's Twitter Profile Photo

Back to wearing clean lab suits again...this time to see the Apollo sample collection (all organised by mission number). Very, very cool! Did the old microscope trick to get a better view of the troctolite. #satisfiedgeologist ⛏#explorationinterns #lunarscience #mineralogy

Back to wearing clean lab suits again...this time to see the Apollo sample collection (all organised by mission number). Very, very cool! Did the old microscope trick to get a better view of the troctolite. #satisfiedgeologist ⛏#explorationinterns #lunarscience
#mineralogy
NASA Astronauts (@nasa_astronauts) 's Twitter Profile Photo

Before going to space, Astronauts go to geology camp! Geology helps us discover information about the early history of the Moon, Earth, and inner solar system. Studying rock and soil samples from the Moon & Mars will be crucial in our journey of human space exploration. #Artemis

Before going to space, Astronauts go to geology camp! Geology helps us discover information about the early history of the Moon, Earth, and inner solar system. Studying rock and soil samples from the Moon & Mars will be crucial in our journey of human space exploration. #Artemis
Natasha (@mantlerocks) 's Twitter Profile Photo

Throwback to “peridotite peak” - part of the ophiolite complex in northern British Columbia. You might be able to spot it on Google Earth! Sad to miss out on field season this year but I’m looking forward to Fiji and Greenland next year! #GeologistsDay #StayAtHome

Throwback to “peridotite peak” - part of the ophiolite complex in northern British Columbia. You might be able to spot it on Google Earth! 

Sad to miss out on field season this year but I’m looking forward to Fiji and Greenland next year! #GeologistsDay #StayAtHome
astrotweeps (@astrotweeps) 's Twitter Profile Photo

Stony-irons are mixtures of metal & silicate rock. Most beautiful are pallasites, with green olivine (peridot) crystals in metal matrix. Their origin is highly debated. Maybe they come from core-mantle interface of a differentiated asteroid, maybe they form by asteroid impacts

Stony-irons are mixtures of metal & silicate rock. Most beautiful are pallasites, with green olivine (peridot) crystals in metal matrix. Their origin is highly debated. Maybe they come from core-mantle interface of a differentiated asteroid, maybe they form by asteroid impacts
nishio (@in12344321) 's Twitter Profile Photo

Our new paper is out!! We studied the formation process of ultra-depleted peridotites #mantle #peridotite doi.org/10.1029/2022JB…

ANZIC (@anzic_iodp) 's Twitter Profile Photo

⏰️ Reminder! Geoscience Australia Seminar 15 mins The New Caledonia Ophiolite Land-to-Sea Drilling Project (SW Pacific): Exploring, on-shore and off-shore, the structure, composition & resources of an exhumed mantle wedge section — Marguerite Godard events.teams.microsoft.com/event/f9890f03…

⏰️ Reminder! <a href="/GeoscienceAus/">Geoscience Australia</a> Seminar 15 mins

The  New Caledonia Ophiolite Land-to-Sea Drilling Project (SW Pacific): Exploring, on-shore and off-shore, the structure, composition &amp; resources of an exhumed mantle wedge section — Marguerite Godard

events.teams.microsoft.com/event/f9890f03…
Romain Tilhac (@romaintilhac) 's Twitter Profile Photo

Europium anomalies kinetically developed without plagioclase: check out our new Nature Communications paper that just came out! dx.doi.org/10.1038/s41467…