1. Sepiolite and Palygorskite in Japan
- Author
-
N. Imai and R. Otsuka
- Subjects
Supergene (geology) ,Sepiolite ,Meteoric water ,medicine ,Mineralogy ,Carbonate rock ,Palygorskite ,Sedimentary rock ,Clay minerals ,Hydrothermal circulation ,Geology ,medicine.drug - Abstract
Recent investigations on palygorskite and sepiolite from Japan are summarized in relation to their mode of occurrence and mineral genesis. Description of the Japanese palygorskites has been confined to only two specimens from the Kuzuu district, represented by “karst region” where a thick sequence of carbonate rocks crops out extensively. These two palygorskites occur along fissures or faults as fillings and are considered to have been formed by direct precipitation from an aqueous solution at earth-surface temperature. The solution rich in silica and magnesium with lesser amount of aluminium, resulted from the descent of meteoric water. Japanese sepiolites, on the other hand, show various modes of occurrence, and may be classified largely into four groups on the basis of their mode of occurrence; (1) sepiolite in serpentinite, (2) sepiolite associated with metallic mineral deposits, (3) sepiolite from the “karst region”, and (4) sepiolite (iron-rich variety) in Tertiary sediments. The sepiolites are considered to be of either hydrothermal or supergene origin, and to have been formed by direct crystallization from low-temperature hydrothermal solution and/or from supergene or marine water rich in silica, magnesium and other components. Palygorskite and sepiolite in Japan do not form sedimentary deposits of economical importance, and occur on a small scale. Intensive studies of clay mineral compositions in clay fractions of surface marine sediments in the oceans and seas in the environs of the Japanese Island Arc, have not confirmed so far the presence of palygorskite or sepiolite.
- Published
- 1984
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