Carbon materials in Antarctic and nonAntarctic carbonaceous chondrites : high-resolution transmission electron microscopy
スポンサーリンク
概要
- 論文の詳細を見る
Carbon materials from eight Antarctic carbonaceous chondrites (CM2, CO3, and CV3 types) and two nonAntarctic carbonaceous chondrites (CM2 and CV3 types) were studied using a high-resolution transmission electron microscope (HRTEM). Nanodiamonds and “carbonaceous globules” were found in seven of the Antarctic chondrites and one nonAntarctic CM2 chondrite. These results suggest that nanodiamonds and carbonaceous globules are common in carbonaceous chondrites. The finding of carbonaceous globules in the meteorites that experienced post-hydration high-temperature thermal metamorphism suggests that they are resistant to thermal metamorphism. Well-crystallized graphite was mainly found in the CV3- and CO3-type chondrites, whereas poorly crystallized graphite was mainly found in the CM2-type chondrites. The CM2-type chondrites also contain characteristic carbon structures that are similar to tetrahedral carbon onions and multilayered fullerene. In this study, we discuss the origin of these types of carbon material.
- 日本鉱物科学会の論文
- 2008-06-01
著者
-
Akai Junji
Department Of Geology Faculty Of Science Niigata University
-
Akai Junji
Department Of Earth Sciences Faculty Of Science Niigata University
-
AOKI Takayuki
Graduate School of Science and Technology, Niigata University
-
Aoki Takayuki
Graduate School Of Science And Technology Niigata University
関連論文
- Crystal orientation analyses of biominerals using Kikuchi patterns in TEM
- Twinned aragonite crystals found in the bivalvian crossed lamellar shell structure
- Calcic analog of clinojimthompsonite ftom the Oeyama Ophiolite,Southwest Japan
- Four-layer orthorhombic polytype (4O) in strontio-joaquinite group minerals found in the Ohmi region, central Japan
- Strontium, barium and titanium-bearing minertals and their host rocks form Ohmi, Japan
- Brockite form Ishikawa, Fukusima Prefectur, Japan
- Shock effects experiments on serpentine and thermal metamorphic conditions in Antarctic carbonaceous chondrite
- HRTEM OBSERVATION OF NEW COMPLEX POLYTYPE OF BIOTITE FROM DACITES IN HIGASHIYAMA HILLS, NIIGATA, CENTRAL JAPAN
- Void structures in olivine grains in thermally metamorphosed Antarctic carbonaceous chondrite B-7904
- TEM observation of void-like defect structures in matrix-and isolated-olivine grains in Allende (CV3)
- Sources of organic carbon and depositional environment in the Bengal delta plain sediments during the Holocene period
- Mineralogical consideration of possible microfossils in martian meteorite ALH84001
- Ultrastructural observations of dental epithelial cells and enameloid during enameloid mineralization and maturation stages in stingrays, Urolophus aurantiacus, an elasmobranch
- T-T-T diagram of serpentine and saponite, and estimation ofmetamorphic heating degree of Antarctic carbonaceous chondrites
- Mineralogical evidence of heating events in Antarctic carbonaceous chondrites, Y-86720 and Y-82162
- Carbon materials in Antarctic and nonAntarctic carbonaceous chondrites : high-resolution transmission electron microscopy
- High resolution electron microscopic characterization of phyllosilicates and finding of a new type with 11Å structure in Yamato-74662
- Calcium distribution in alkali feldspar of a quartz syenite from Cape Ashizuri, Shikoku, southwest Japan
- Mineralogical study of matrix- and groundmass-phyllosilicates, and isolated olivines in Yamato-791198 and -793321: With special reference to new finding of 14 Å chlorite in groundmass