Caymanite
| Caymanite | |
|---|---|
 Caymanite from Cayman Brac, Cayman Islands | |
| General | |
| Category | Carbonate minerals |
| Formula (repeating unit) | CaMg(CO3)2 |
| Identification | |
| Color | white to red and black |
| Solubility | Poorly soluble in dilute HCl |
Caymanite at its type area is an uncommon variety of dolomite, also known as dolostone, originally reported from locations in the Miocene Cayman Formation[1] in the Cayman Islands: the Bluff in Cayman Brac and the East End on Grand Cayman.
Geology
Away from the type area, material now being called "caymanite" is not an "uncommon variety of dolostone" as it is sensu stricto at the type area. It has been reported from the Buda Hills of Hungary.[2] Caymanite occurs as a fine grained or vug filling variety of the mineral dolomite CaMg(CO3)2. It occurs as white to red and black filling in fossil molds, small cavities and caves.[3] It is used as a semi-precious stone. In New South Wales, Australia, pockets of later-deposited beds (usually reddish) are widespread in the Silurian-Devonian limestones. These are thus far reported only from the Lachlan Fold Belt portion of the Tasman orogenic zone. They are mostly small pockets but occasionally reach up to several metres wide. These had been long known about and began to be referred to as Caymanite by Dr. Armstrong Osborne who also worked up and published the finding that the Jenolan cave complex is world's oldest known and dated open cave system. The best description so far of the New South Wales caymanite is from Jenolan Caves. None of the NSW material is silicified or in any way suitable for use as a semi-precious stone.
Formation
The formation of caymanite followed two phases. The first phase of caymanite formation occurred after deposition, lithification, and karst process of the Oligocene Cayman Member. The second phase of caymanite formation occurred after joints had developed in the Middle Miocene Pedro Castle Member. Caymanite deposition predated dolomitization, a process where limestone is altered from contact with magnesium-rich water. Then the magnesium carbonate replaces the calcite naturally in the rock without complete destruction of the original sedimentary fabrics or structures. Dolomitization in the Bluff Formations of Cayman Brac occurred 2-5 million years ago.[4]
References
- ^ Brian Jones and Robert W. Luth, Petrography of Finely Crystalline Cenozoic Dolostones as Revealed by Backscatter Electron Imaging: Case Study of the Cayman Formation (Miocene), Grand Cayman, British West Indies, Journal of Sedimentary Research; November 2003; v. 73; no. 6; p. 1022-1035; doi:10.1306/042303731022
- ^ L. Korpása, M. Lantosa and A. Nagymarosy, Timing and genesis of early marine caymanites in the hydrothermal palaeokarst system of Buda Hills, Hungary, Sedimentary Geology, Volume 123, Issues 1-2, January 1999, Pages 9-29 doi:10.1016/S0037-0738(98)00090-6
- ^ Brian Jones and Ian G. Hunter, The Oligocene-Miocene Bluff Formation on Grand Cayman, Caribbean Journal of Science, Vol. 25, No. 1-2, 71-85, 1989 [1]
- ^ Suzanne M. Pleydell, Brian Jones, F. J. Longstaffe, H. Baadsgaard, Dolomitization of the Oligocene–Miocene Bluff Formation on Grand Cayman, British West Indies, Canadian Journal of Earth Sciences, 1990, 27:1098-1110, 10.1139/e90-114