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Click the microscope button to view a thin section for this sample Only 5% of the outer surface of lew 88516 still had a black fusion crust. This cumulate gabbroic rock (lherzolite) was found in 1988 in the lewis cliffs region of antarctica
Isotopic techniques have dated it at 166±16 m.y The observation of high carbon content in lew 88516,13 highlights the extreme difficulty of trying to obtain representative samples of whole meteorites for this kind of investigation. Pitted and mostly shiny fusion crust covers 80% of lew88516
The sample's interior consists of green/black matrix which appears glassy and has conchoidal fractures
Several dark colored inclusions are present. Lew88516 was a small nondescript meteorite that was not recognized as an achondrite until it was broken open hence, it waited 2 years to be processed in numerical order According to satterwhite and mason (1991), lew88516 had a “pitted and mostly shiny fusion crust over 80 % of the surface.” preliminary examination of the thin section showed about 50 % olivine, 35 % pyroxene, 8 %. In this paper, we pay attention to amphiboles in martian meteorites that are very important phases for understanding martian igneous processes involving water contents of magmas and atmospheric evolution of the red planet.
Comparison of the lew88516 and alha77005 martian meteorites Similar but distinct by mineral and bulk compositions, the lewis cliff (lew) 88516 meteorite is quite similar to the alha77005 martian meteorite. Cliffs 88516 is a gabbroic lherzolite with geochemical and petrologic characteristics typical of the shergottites, a distinct subgroup of basaltic achondrites belonging to the snc (martian) meteorite clan. Snc meteorite is an acronym for shergottite nakhilite chassignite plutonic rock has solidification mechanism has solidification timescale rock has part mineral has texture has genesis achondrite has distinguishing feature next antarctic meteorite
Antarctic meteorite, lherzolite shergottite previous antarctic meteorite
D'un point de vue pétrographique, lew 88516 est une péridotite à gros grains, et elle a donc été classée parmi les shergottites lherzolitiques.
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