the cheshin meta-calcareous rocks (permo triassic) in southeast hamedan outcrop in association with a variety of pelitic schists and hornfels rocks. the intrusion of the alvand batholith (jurassic age) into pelitic and calcareous host rocks has produced metamorphic rocks in the hamedan area (cheshin village). on the basis of the dominance of calcite/dolomite, silicate and ore minerals, the calc...

The Sanchahe iron-gold deposit in western Shandong province is located the southeast of North China Craton. skarn type (without copper) contact belt between pyroxene diorites and Ordovician limestone xenoliths. zircon U-Pb age 138.4 ± 1.2 Ma belonging to Early Cretaceous. Pyroxene (Rittmann index ? = 2.2~2.5) belong calc-alkaline series SiO2 content 55~59%. Furthermore, are characterized by hig...

the dehbid magnetite deposit is located in northeastern part of fars province, in the southern border of sanandaj-sirjan metamorphic zone. the mineralization occurred as veins and lenses along nw-se faults. the ores are mainly hosted in silicified dolomite of early mesozoic (triassic). mineralogical studies show that the ores are dominated by magnetite and minor hematite with massive texture oc...

When the minimal renal threshold for blood hemoglobin is exceeded there is observed a deposit of iron staining pigment in the epithelium of the renal convoluted tubules. At a certain point this epithelium cannot take up more hemoglobin and this coincides with the minimal renal threshold level. When the injections of blood hemoglobin are kept below the minimal renal threshold level we note a com...

Distal skarns form by the metasomatic reactions of a host rock induced far-traveled hydrothermal fluids. Physical and structural characteristics geochemical patterns distal PbZn skarn bodies were studied at Petrovitsa deposit in southern Bulgaria. Skarn formed from interaction fluids with reactive lithologies (marble gneiss). These transported along sub-vertical feeder structures lithological c...