Scientific Quarterly Journal of Geosciences

Scientific Quarterly Journal of Geosciences

Textural and Structural Investigation on the Chromite deposition Gaft and Foromad Areas, Sabzehvar

Document Type : Original Research Paper

Authors
1 Ministry of Education, District One, Mashhad, Iran
2 Department of Geology, Faculty of Sciences, University of Shahid Bahonar, Kerman, Iran
Abstract
This paper deals with on the most important kind of structures and textures of the chromite deposits in Goft and Foromad areas of Sebzehvar for the first time. The area under investigation is situated in the most westerly part of Sebehvar Ophiolitic Belt and north-west of the town of Sabzehvar. It consists of several pencil-shaped, lenticular and layered chromite deposits, with varying dimensions, in serpentinized ultrabasic rocks, most of which are serpentinized harzburgite.
With regards to the results obtained from this investigation, the structure and texture present in the area may be divided into two principal groups:
1.  Initial textures and structures.
2. Secondary textures and structures.
Among the most important initial structures and textures, one may hint at, their scattered, reacting, accumulating, inter - accumulating, reticulate, vermicular, nodular, skeletal, massive, dense, banded and cross-bedded properties. Whereas, the secondary textures and structures constitutes various types of strains, cataclastics, mylonitization, brecciation, folding and faulting and ultimately supergene and island-like.
The initial textures and structures, all are resulted from crystallization, accumulation and precipitation of chromite accompanied with silicates of olivine and pyroxene, at various stages of crystallization and basaltic magma. While the secondary ones are formed from deformation and contortion caused by tectonic and non-tectonic phenomena.
Thus, the above-mentioned points are of utmost importance in exploration and exploitation of chromites.
Keywords

Subjects


 
Alavi Tehrani, N., 1977- Geology and petrography in the Ophiolite range NW of Sabzevar (Khorassan/Iran), with special regard to metamorphism and genetic relations in an ophiolite suite, (Ph. D. thesis), Geological Survey of Iran, Report No. 43, 156p.
Baroz, F., et al., 1983, Ophiolites and related formations in the central part of the Sabzevar range (Iran) and possible geotectonic reconstructions: Geodynamic Project (Geotraverse) in Iran, Report No. 51, Geological Survey of Iran, 205-238.
Bernardt, U., 1983- Middle- Tertiary volcanic rocks from the Southern Sabzevar Zone, Khorassan (NE Iran): Geodynamic Project (Geotraverse) in Iran, Geological Survey of Iran, 277-284.
Deifenbach, K. W., 1988- Chromite mineralization, genesis and exploration: Second Mining Symposium, Kerman- Iran, 16-35.
Duke. J. M., 1990- Magmatic segregation deposits of chromite: Ore deposit models, Geological Association of Canada Publications, 133-144.
Green baum, D., 1977- The chromitiferous rocks of the Troodos Ophiolite Complex, Cyprus: Economic Geology, 72(7), 1175-1194.
Leblanc, M., and Ceuleneer, G., 1992- Chromite crystallization in a multicellular magma flow: Evidence from a chromitite dike in the Oman Ophilite: Lithos, 27, Elsevier Science Publishers, 231-257.
Lendsley, D. H., Rumble, D., Haggerty, S., Goresy, A., and Huebner, J., 1976 Oxide minerals: Mineralogical Society of America, Short Course Notes, vol.3, Southern Printing Company, p. Hg 101- Hg 279.
Nicolas, A., et al., 1981- Structural classification of chromite pods in Southern New Caledonia: Economic Geology, 76(4), 805-831.
Ramdohr, p. 1980- The ore minerals and their intergrowth: Sec. edition, English translation of the 4th. edition, Pergamon press, 946-955.
Thayer, T. P. 1964, Principal features and origin of podiform chromite deposits, and some observations on the Guleman, Turkey: Econ. Geol. vol. 59, 1497-1524.
Volume 6, 23-24
Spring & Summer 1998, Vol. 6, No. 23-24
Autumn 1998
Pages 40-56