The olivine-phyric shergottite LAR12011 was
found at Larkman Nunatuk during the 2012 ANSMET expedition
[1]. The preliminary analysis of LAR12011 presented in [1] and
oxygen isotope analysis in [2] confirms its Martian origin. This
new sample is paired with LAR06319 [1-3]. Here, we present
petrography and new data on the trace element chemistry of
LAR12011
