LL chondrite


The LL chondrites are a group of stony meteorites, the least abundant group of the ordinary chondrites, accounting for about 10–11% of observed ordinary-chondrite falls and 8–9% of all meteorite falls. The ordinary chondrites are thought to have originated from three parent asteroids, with the fragments making up the H chondrite, L chondrite and LL chondrite groups respectively. The composition of the Chelyabinsk meteor is that of a LL chondrite meteorite. The material makeup of Itokawa, the asteroid visited by the Hayabusa spacecraft which landed on it and brought particles back to Earth also proved to be type LL chondrite.

Name

LL stands for Low iron, Low metal.

Chemical composition

They contain 19–22% total iron and only 0.3–3% metallic iron. That means that most of the iron is present as iron oxide in the silicates; olivine contains 26 to 32 mol% fayalite. The most abundant minerals are hypersthene and olivine. Other minerals include Fe–Ni, troilite, feldspar or feldspathic glass, chromite, and phosphates.

Structural composition

LL chondrites contain the largest chondrules of the ordinary chondrite groups, averaging around diameter.
The LL group includes many of the most primitive ordinary chondrites, including the well-studied Semarkona chondrite. However, most LL chondrites have been thermally metamorphosed to petrologic types 5 and 6, meaning that their minerals are homogeneous in composition and chondrule borders are difficult to discern.
This, together with the low content of metal, led the 19th century mineralogist Tschermak to determine that they formed a transitional stage between chondrites and achondrites and to name them amphoterites. We know now that LL chondrites and achondrites are quite different, so this name is no longer in use.
Many of the LL chondrites are breccias.