Mantle Rock Drilled Up in Cores

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Researchers aboard the JOIDES Resolution have successfully drilled over 1 kilometer below the seabed in the mid-Atlantic Ocean, collecting a core primarily composed of peridotite, a type of upper mantle rock. This achievement has generated significant interest among scientists, particularly regarding the potential classification of the rocks as true mantle samples. Some experts suggest that the presence of seawater influence may indicate these samples are more representative of deep crust rather than the mantle. However, the petrology remains noteworthy. As drilling progresses, the team is uncovering fresher mantle rock that has not melted into magma, providing valuable insights into the processes of magma formation and flow, which could enhance understanding of volcanic activity globally. The core samples also revealed veins of asbestos, prompting the implementation of additional safety measures during research.
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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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