In 1986, during a survey of the borate veins at Fuka Mine, Fuka, Okayama
Prefecture, Japan, some small blue-violet crystals were observed closely
associated with pentahydroborite. This new mineral was named Henmilite
after Prof. Kichinosuke Henmi and his daughter Dr. Chiyoko Henmi, Department
of Earth Science, Okayama University. In that find, crystal sizes were
so small (maxium 0.2mm) and specimens recovered were so scarce that some
mineralogical properties could not be mesured. In 1992, the mineral was
found in a calcite vein cutting gehlenite-spurrite skarns at the Fuka Mine,
this time as prismatic crystals up to 3mm long. This new material provided
ample opportunity to completely describe the crystallography of the species
. In 2003, a new deposit was found and amazing specimens were recovered
until the deposit is now almost exhausted. The entry to the mine is
prohibited by the property owner. The specimen above is one of those found
in early years.
Henmilite is a very fragile mineral. / Mohs Hardness: 3 / Density g/cm3 / On heating the mineral at 900°C, tenorite (Cuo) and calcium borate (Ca2BsO5) appear as crystalline phases.
1986年に岡山県布賀において世界で初めて発見された新鉱物です。非常に小さい結晶ですが、マクロで撮ると美しい紫色をしていることがよくわかります。低温の熱水作用によってできるカルシウムと銅の含水ホウ酸塩鉱物で、紫〜青色の皮膜や顕微鏡サイズの微小な結晶の形をとります。 |