Inner Mongolia

Inner Mongolia
Sposób odkryciaspadły
Państwo Chiny
Miejsce znalezieniaregion autonomiczny Mongolia Wewnętrzna
Data znalezienia1962 lub 1963
Masa3 kg
Typmeteoryt kamienny, chondryt
Klasaoliwinowo-hiperstenowy
GrupaL6
Położenie na mapie Chin
Mapa konturowa Chin, blisko centrum na prawo znajduje się punkt z opisem „Inner Mongolia”
Ziemia41°00′00″N 112°00′00″E/41,000000 112,000000

Inner Mongolia (inne nazwy: Inner Monglia, Nei Monggol) – meteoryt kamienny należący do chondrytów oliwinowo-hiperstenowych L 6, którego spadek zaobserwowano w 1962 lub 1963 roku w regionie autonomicznym Mongolia Wewnętrzna, na północy Chin. Z miejsca spadku pozyskano 3 kg masy meteorytowej.

Bibliografia

Media użyte na tej stronie

China edcp location map.svg
Autor: Uwe Dedering, Licencja: CC BY-SA 3.0
Location map of China.

EquiDistantConicProjection : Central parallel :

  • N: 36.0° N

Central meridian :

  • E: 104.0° E

Standard parallels:

  • 1: 30.0° N
  • 2: 42.0° N

Latitudes on the central meridian :

  • top: 57.0° E
  • center: 37° 29′ N
  • bottom: 17.96° N
Made with Natural Earth. Free vector and raster map data @ naturalearthdata.com.
Orange pog.svg
Shiny orange button/marker widget.
Iron-150475.jpg
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
Iron (Var.: Kamacite)
Locality: Nantan meteorites (Nandan meteorites), Lihu - Yaochai area, Nandan County, Hechi Prefecture, Guangxi Zhuang Autonomous Region, China (Locality at mindat.org)
Size: 7.9 x 4.2 x 3.9 cm.
A LARGE meteorite from a witnessed fall! From the accompanying literature: "Nantan iron meteorites represent one of the rare witnessed iron meteorite falls in the world. The fall was vividly recorded (in Chinese records): “During summertime in May of Jiajing 11th year, stars fell from the northwest direction, five to six fold long, waving like snakes and dragons. They were bright as lightning and disappeared in seconds. These records show the meteorite to have fallen in the year 1516 AD. The fall site was not discovered until much later, in 1958. The specimens have a coarse octahedral structure, and contain 92.35% iron and 6.96% nickel, belonging to IIICD classification of Wasson et al (1980’s).” This is a VERY LARGE one, weighing 223 grams!