Mineral Database
Magnesiohornblende
Magnesiohornblende crystals from altered diorite from the Sarn Complex, Ll?n. Viewed under the microscope in crossed polarized light. National Museum of Wales specimen (NMW 93.12G). © National Museum of Wales.
- Silicates
- Hydrothermal
- Metamorphic
magnesiohornblende is an amphibole, more specifically a calcic amphibole which occurs as a rock-forming mineral in basic igneous rocks and as amphibolite grade metamorphic rocks.
as with many other ferro-magnesian minerals, magnesiohorneblende has only been confirmed from a few localities in Wales, and there are even fewer analyses presented in the literature. It is quite likely that it is more abundant than these reports reflect.
- Aberbach, Pembrokeshire: the Llech Dafad Intrusion, of Ordovician age, exposed to the northeast of Aberbach, Pembrokeshire contains green pleochroic magnesiohornblende forming needle-like crystals. These crystals over print clinopyroxene and replace the groundmass and are therefore interpreted as sub-solidus in origin (Bevins, 1979).
- Llŷn, Gwynedd: magnesiohornblende occurs within the basic rocks of the Precambrian Sarn Complex, exposed in scattered outcrops on Llŷn. The amphibole has several textural forms; as small anhedral crystals interstitial to plagioclase; as thin rims around clinopyroxene; and as subhedral clinopyroxene-free crystals. Whereas the amphibole in the sheared rocks clearly has a subsolidus origin that in the unsheared dioritic rocks may be either post-magmatic or late-stage magmatic (Horák, 1993).
- The geology of the Strumble Head-Fishguard region, Dyfed, Wales. Unpublished Ph.D. thesis, University of Keele, 256pp.
- The Late Precambrian Coedana and Sarn Complexes, Northwest Wales - a Geochemical and Petrological study. Unpublished Ph.D. thesis, University of Wales, 415pp.
- A FORTRAN program for the classification of amphiboles according to IMA (1978). IGS Petrographic Report 560124 (unpublished).