Mantle Rock Drilled Up in Cores

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This month, researchers aboard the JOIDES Resolution, part of the International Ocean Discovery Program (IODP), successfully drilled over 1 kilometer below the seabed in the mid-Atlantic Ocean, retrieving a core primarily composed of peridotite, a type of upper mantle rock. While some debate exists regarding the classification of these samples as true mantle material due to seawater influence, the petrology remains significant. Researchers, including Jessica Warren and Vincent Salters, emphasize the importance of these samples for understanding magma dynamics and volcanic processes. The presence of asbestos in the cores has prompted the implementation of additional safety protocols.

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  • Understanding of mantle geology and petrology
  • Familiarity with drilling techniques used in oceanography
  • Knowledge of geochemical processes related to magma formation
  • Awareness of safety protocols in geological fieldwork
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  • Research the geological significance of peridotite in mantle studies
  • Explore the methodologies of the International Ocean Discovery Program (IODP)
  • Learn about the implications of asbestos in geological samples
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Geologists, geochemists, oceanographers, and researchers interested in mantle dynamics and volcanic activity will benefit from this discussion.

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As reported in Science magazine, so maybe pay-walled.

This month, researchers onboard the JOIDES Resolution, the flagship of the International Ocean Discovery Program (IODP), say they have finally succeeded. Drilling below the seabed in the mid–Atlantic Ocean, they have collected a core of rock more than 1 kilometer long, consisting largely of peridotite, a kind of upper mantle rock.

Researchers on land are eagerly following the ship’s daily scientific logs as it continues to drill, says Jessica Warren, a mantle geochemist at the University of Delaware.

There’s still some room for debate about whether the rocks are a true sample of the mantle, says Donna Blackman, a geophysicist at the University of California, Santa Cruz. The seismic speedup at the Moho is thought to reflect the lack of water or calcium and aluminum minerals in mantle rocks. Because the samples still show some influence of seawater, Blackman says she might classify them as deep crust. “But the petrology is interesting and special regardless,” she says. And as the team continues drilling into deeper rocks, Lissenberg says, “They’re getting fresher.”Indeed, it appears the team is already sampling mantle rock that has never melted into magma, which then cools and crystallizes into different kinds of crustal rocks, says Vincent Salters, a geochemist at Florida State University. By capturing the rock at this point, he says, researchers should be able to learn how magma melts, flows, and separates—clues to the workings of volcanoes worldwide.
A petrologist examines an intact section of mantle rock

The rock cores contained veins of asbestos, necessitating extra safety protocols.Lesley Anderson/U.S. Antarctic Program & IODP
 
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BillTre said:
As reported in Science magazine, so maybe pay-walled.
It looks like marble! Wow!
 

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