A Unique Chondrite Clast in the NWA 13262 (L3 Breccia) Bearing Similarities to Carbonaceous and Ordinary Chondrites

In ordinary chondrites (OC) a large diversity of dark-colored clasts (or inclusions) can be found; however, these terms do not provide any information about the genetic origin and the mineralogy of the fragments and encompass very different types of rocks summarized in [1]. Most clasts within OC breccias probably derived from projectiles, whereas other may have been included by early accretion. Here, we report on a chondritic clast that is different from material sampled by individual meteorites.