Add to ORKGThe Tenth Symposium on Polar Science/Special session: [OA] Antarctic meteorites, Thur. 5 Dec. / 3F Multipurpose conference room, National Institute of Polar Researc
Most Martian meteorites are heavily shocked, exhibiting numerous shock features, for example undulat...
Among 4100 meteorite samples found around the Yamato Mountain area during the field season of 1998-1...
This project describes two Martian meteorites, paired olivine-phyric shergottites LAR 12240 and LAR ...
Asuka (A) 12325 is the first poikilitic shergottite having a depleted pattern in light rare earth el...
The Tenth Symposium on Polar Science/Special session: [OA] Antarctic meteorites, Thur. 5 Dec. / 3F M...
The 13th Symposium on Polar Science/Ordinary sessions [OA] Antarctic meteorites, Thu. 17 Nov
Y980459, a new Martian meteorite from Antarctica, is composed of coarse porphyritic olivine grains (...
Y980459 is a new type of shergottite, consisting mainly of olivine, orthopyroxene with augite mantle...
Martian meteorites are the only samples currently available on Earth to study Mars. Most martian met...
Shock metamorphism is one of the most fundamental processes in the history of Martian meteorites, es...
NWA 6342 is an intermediate, ultramafic, poikilitic shergottite that was found in Algeria in 2010. A...
AbstractYamato 984028 (Y984028) is a newly identified lherzolitic shergottite, recovered from the Ya...
The study of shock-metamorphic features of the Zagami meteorite revealed pseudotachylite-like melt v...
Mineralogical and petrologic study on the Y-793605 lherzolitic shergottite using an optical microsco...
Knowledge of Martian igneous and mantle compositions is crucial for understanding Mars’ mantle evolu...
Most Martian meteorites are heavily shocked, exhibiting numerous shock features, for example undulat...
Among 4100 meteorite samples found around the Yamato Mountain area during the field season of 1998-1...
This project describes two Martian meteorites, paired olivine-phyric shergottites LAR 12240 and LAR ...
Asuka (A) 12325 is the first poikilitic shergottite having a depleted pattern in light rare earth el...
The Tenth Symposium on Polar Science/Special session: [OA] Antarctic meteorites, Thur. 5 Dec. / 3F M...
The 13th Symposium on Polar Science/Ordinary sessions [OA] Antarctic meteorites, Thu. 17 Nov
Y980459, a new Martian meteorite from Antarctica, is composed of coarse porphyritic olivine grains (...
Y980459 is a new type of shergottite, consisting mainly of olivine, orthopyroxene with augite mantle...
Martian meteorites are the only samples currently available on Earth to study Mars. Most martian met...
Shock metamorphism is one of the most fundamental processes in the history of Martian meteorites, es...
NWA 6342 is an intermediate, ultramafic, poikilitic shergottite that was found in Algeria in 2010. A...
AbstractYamato 984028 (Y984028) is a newly identified lherzolitic shergottite, recovered from the Ya...
The study of shock-metamorphic features of the Zagami meteorite revealed pseudotachylite-like melt v...
Mineralogical and petrologic study on the Y-793605 lherzolitic shergottite using an optical microsco...
Knowledge of Martian igneous and mantle compositions is crucial for understanding Mars’ mantle evolu...
Most Martian meteorites are heavily shocked, exhibiting numerous shock features, for example undulat...
Among 4100 meteorite samples found around the Yamato Mountain area during the field season of 1998-1...
This project describes two Martian meteorites, paired olivine-phyric shergottites LAR 12240 and LAR ...