Ooids in thin section.
Ooids are spherical bodies of calcium carbonate with an internal structure of concentric layers. Its nucleus can be a fragment of other carbonate material or clastic sediment.

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Ooids in thin section.
Ooids are spherical bodies of calcium carbonate with an internal structure of concentric layers. Its nucleus can be a fragment of other carbonate material or clastic sediment.
ooids & Jurassic oyster.
Science under cut
ooid with sparry isopachous cement, its a cut surface surface (notice the ooids are sliced, indicating boring on a beach hardground))
Crystalline top is low-Mg oyster shell (perpetrator of said boring)
((Brown plain polar, grey is crosspolar))
Stuid the ooid geology themed shirts, get one at the link below. https://everpress.com/stuid-the-ooid
Internal lamination with syn-depositional deformation in a 1. 3 billion year old #iron #silicate #ooid, this means the ooid was still soft and squishy when it was buried. Veiw is ~1 mm across #geology #precambrian #mesoproterozoic https://www.instagram.com/p/Bw4B5zCJxC3/?utm_source=ig_tumblr_share&igshid=d9cf3pd7yw0f
Ooid Wednesday But what is an ooid? Ooids are spheroidal sedimentary grains composed of calcium carbonate or iron such as these ooids from a banded iron formation.