- 【Updated on May 12, 2025】 Integration of CiNii Dissertations and CiNii Books into CiNii Research
- Trial version of CiNii Research Knowledge Graph Search feature is available on CiNii Labs
- Suspension and deletion of data provided by Nikkei BP
- Regarding the recording of “Research Data” and “Evidence Data”
Bi-bearing secondary minerals from the Kinkei mine, Chino City, Nagano Prefecture, Japan
-
- Harada Akira
- Friends of Minerals, Tokyo
-
- Yamada Takashi
- Friends of Minerals, Tokyo
-
- Matsubara Satoshi
- National Museum of Nature and Science
-
- Miyawaki Ritsuro
- National Museum of Nature and Science
-
- Shigeoka Masako
- National Museum of Nature and Science
-
- Miyajima Hiroshi
- Fossa Magna Museum
-
- Sakurai Hiroshi
- Min. Soc. Nagoya
Bibliographic Information
- Other Title
-
- 長野県茅野市金鶏鉱山産ビスマスの二次鉱物
Description
Bi-bearing secondary minerals such as dukeite and waylandite occur in small cavities of quartz vein from the Kinkei mine, Chino City, Nagano Prefecture, Japan. The quartz vein belongs to Sanbagawa metamorphic rocks and is characterized in association with chromite, Cr-bearing green muscovite and chromian dravite. Minor constituents are gold, bismuth, tellurobismuthite, gersdorffite, rutile, phosphates (florencite-(Ce), monazite-(Ce), xenotime-(Y) ), and andalusite. Dukeite forms hemispherical aggregate up to 2mm diameter composed with thin lamellar crystals associating with rhombohedral waylandite. These secondary minerals are produced by the decomposition of chromite, phosphates and Bi minerals.
Journal
-
- Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences
-
Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences 2010 (0), 75-75, 2010
Japan Association of Mineralogical Sciences
- Tweet
Details 詳細情報について
-
- CRID
- 1390282680521468800
-
- NII Article ID
- 130004601723
-
- Text Lang
- ja
-
- Data Source
-
- JaLC
- CiNii Articles
-
- Abstract License Flag
- Disallowed