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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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East Africa
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Kenya
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Mount Kenya (1)
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North Africa
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Morocco
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Rif
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Beni Bouchera (1)
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Sahara (1)
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Southern Africa
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Kaapvaal Craton (1)
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Karoo Basin (1)
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South Africa
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Bushveld Complex (1)
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Cape Province region (1)
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Mpumalanga South Africa
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Barberton South Africa (1)
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Witwatersrand (1)
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West Africa
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Ivory Coast (1)
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Antarctica
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Victoria Land
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Asia
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Kazakhstan
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Far East
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China
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Russian Federation
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fluorine (1)
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hydrogen
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D/H (2)
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isotope ratios (27)
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isotopes
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C-14 (1)
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stable isotopes
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C-13/C-12 (8)
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D/H (2)
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O-17/O-16 (3)
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O-18/O-16 (7)
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Os-188/Os-187 (2)
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Pb-207/Pb-206 (2)
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iron (1)
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rare earths
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oxygen
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fossils
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Invertebrata
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microfossils (4)
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Glossopteris flora (1)
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geochronology methods
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geologic age
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upper Quaternary
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Tertiary
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upper Oligocene
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Paleocene
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Paleocene-Eocene Thermal Maximum (1)
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Mesozoic
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Paleozoic
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upper Paleozoic (1)
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upper Precambrian
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Sinian
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Witwatersrand Supergroup (2)
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igneous rocks
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turbidite (2)
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meteorites
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meteorites
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iron meteorites
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octahedrite
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micrometeorites (1)
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stony irons
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stony meteorites
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shergottite (3)
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ureilite (3)
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chondrites
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carbonaceous chondrites
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Tagish Lake Meteorite (4)
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ordinary chondrites
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rumurutiites (1)
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Yamato Meteorites (1)
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minerals
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native elements
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rutile (1)
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phosphates
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orthopyroxene
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framework silicates
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orthosilicates
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zircon group
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sorosilicates
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sheet silicates
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sulfates
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sphalerite (1)
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troilite (1)
-
-
-
Primary terms
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absolute age (10)
-
Africa
-
East Africa
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Kenya
-
Mount Kenya (1)
-
-
-
North Africa
-
Morocco
-
Rif
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Beni Bouchera (1)
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Sahara (1)
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Southern Africa
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Kaapvaal Craton (1)
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Karoo Basin (1)
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South Africa
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Bushveld Complex (1)
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Cape Province region (1)
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Mpumalanga South Africa
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Witwatersrand (1)
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West Africa
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Ivory Coast (1)
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Antarctica
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Antarctic ice sheet
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East Antarctic ice sheet (1)
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Queen Maud Land
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Sor-Rondane Mountains (1)
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Transantarctic Mountains
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Beardmore Glacier (1)
-
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Antarctic Search for Meteorites Program
Abstract A Japanese field party (Japanese Antarctic Research Expedition 10 (JARE-10)), traversing in the Yamato Mountains of Antarctica in December 1969, recovered nine meteorite masses from ice-field surfaces. These meteorite masses were of diverse types, a fact that set in motion systematic searches for further meteorites. This was initiated by the JARE-15 field party in the austral summer of 1974, which recovered 663 meteorite masses from the ice fields. So many finds led to a hypothesis explaining the unusual concentration of meteorites on the Antarctic ice fields, and later parties searched systematically, according to this hypothesis. The JARE-20, JARE-29, JARE-39 and JARE-41 field parties collected 3692, 1949, 4148 and 3581 meteorite masses in repeated searches, respectively. A total of 15 741 masses is now held by the National Institute for Polar Research, and includes many rare classificatory types, lunar-sourced meteorites and meteorites widely accepted as of martian origin. The original find of nine meteorites triggered the extensive search programmes for meteorites by Japanese and American scientists both in the Yamato Mountain region and the Trans Antarctic Range region of Antarctica.