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Calcite

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Lustrous mostly gemmy twinned crystals of calcite in a cluster without matrix. This is in really good condition. From the late 1990s.The Leiping Mine, situated in Guiyang County of Hunan Province, China, is a significant lead-zinc-silver deposit located within the prolific Nanling Mineral Belt. Geologically, it is characterized by hydrothermal mineralization and skarn formation where Mesozoic granitic intrusions contacted Upper Paleozoic carbonate rocks. This environment provided the ideal conditions for the development of exceptional mineral crystals, most notably the world-class twinned calcite specimens for which the locality is famous. These calcites often occur as large, sharp, heart-shaped (butterfly) twins or complex flattened rhombohedra with superb luster and transparency. Historically, while the region has a long history of mining, modern industrial development at Leiping intensified during the mid-20th century, with the mine serving as a major producer of base metals throughout the 1960s and 1970s. Since the late 1990s, the mine has gained significant international acclaim in the mineralogical community as a premier source for these distinct and highly aesthetic calcite twins.

Product details

SpeciesCalcite
SizeMiniature
Dimensions4.0 x 3.7 x 1.5 cm
Added on05/03/2026

Known provenance

DateCollectorAcquisition price
05/2026Unknown Owner$125.00
Weinrich MineralsNot disclosed

Learn more

Calcite
Mineral guide
Learn about Calcite
diverse shapes, colors, and optical quirks; widely available yet scarce elite pieces from Elmwood and Charcas drive collecting value and display.
Calcite
Regional guide
Calcite from Leiping Mine, China
from Leiping Mine, in the Leiping area of Guiyang County, Chenzhou, Hunan, is one of the unmistakable modern Chinese calcite styles: lustrous, sharp, often translucent to gemmy crystals animated by warm iron-oxide and hematite color. The best specimens do not rely on size alone. They have architecture—wing-like twins, stacked rhombs, spiky scalenohedral sprays, and multi-generation crystals where clear late calcite wraps or caps an older, rust-red included core.