بررسی الگوی کانی سازی در کانسار سلستیت دشت آهو (شهرستان بهمئی) با استفادهاز شواهد زمین شناسی، کانی شناسی و ساخت و بافت کانسنگ

Silicate's deposits in Dasht (plain) Ahoo area in the Kohgiloyeh and Boyerahmad located at the north west of Behbahan and west of Bamaee. The area is constructed with the calcareous rocky horizons which is the main place Mishan and consisted of exposed lenses in the mentioned area. Solicits layers are consisted of silicate crystal small grains which is continued up to the Dasht (plain) and are shown in different types of carbonated back grounds. Silicate grains of sugar like ( crystal) together with carbonates incorporates is the sign of silicate instead of calcium in the calcium sulfate and calcium carbonate. The amount of SrO and So3 are highly correlated (1). Mining constructive fluid most probably have been constituted by the sea water evaporation in a SABKHA place. As these brines enter the bottom sediments, a noticeable amount of Stransuim will be washed from the deposits. When these fluids which are rich with STRANSUIM are discharged in the surface layers which consisted Carbonate materials and ZHIPS, deposit of Silicate will take place by the substitute minerals available and also by the mineral constructive fluid mixtures with Brines rich of sulfate that are locked in the internal layers.

Keywords:

silicate deposit , Api genetic , Mishan constructive , substitute , delaying DEYAGINE