塔里木盆地塔中地区下奥陶统白云岩成因

塔里木盆地塔中地区下奥陶统白云岩广泛发育,岩石类型复杂多样,主要包括结晶白云岩、残余颗粒白云岩、残余灰质白云岩、藻云岩、亮边雾心白云岩、环带白云岩及少量膏云岩等结构类型。白云岩交代现象明显,δ18O普遍为中—高负值（-3.2‰～-8.7‰）;δ13C值基本为低中负值（-3‰～-0.77‰）,Z值大多集中在118～123...

Genesis of Lower Ordovician Dolomite in Central Tarim Basin

Lower Ordovician dolomites in the central Tarim basin are of various types and extensively distributed. Seven dolostone types could be documented based on fabrics and structures, which are crystalline dolomite, residual grain dolomite, residual calcite dolomite, algal dolomite,cloudy centers and clear rims dolomite, clitellum dolomite and gypes dolomite. It's characterised by middle high δ18O negative value（ 3.2%~ 8.7‰）, low middle δ13C negative value（ 3%~ 0.77‰）, and high Z value of 118~123. Most diagenetic temperature calculated by empirical formulas using δ18O values are between 118 to 123℃, which indicates that the temperature degree of dolomitization is low, and so the kind of dolomite belongs to low temperature dolostone. These dolomites have also characteristics of low Mg/Ca and variable Fe/Mn ratio values. According to mineral composition analyzed by electron microprobe, dolomite monomineral can be divided into high Fe content and low Fe content species. 87Sr/86Sr ratios of most samples are low( among 0.708 8~0.709 7), which are similar to seawater strontium isotope composition, and some are of high ratios between 0.710 1 and 0.710 9. These characteristics reveal that the origin of dolomite in the study area can be classified into penecontemporaneous dolomitization and burial dolomitization. According to Ordovican palaeogeographical evolution, the penecontemporaneous dolomitization arised in the seafloor environment, mainly in tidal flats or beach environment. And this kind of dolomite characterised by low diagenetic temperature, low 87Sr/86Sr ratios, and low Fe content dolomite minerals. The burial dolomitization can be interpreted by two diagentic models. One is seepage reflux dolomitization during early shallow burial stage and characterised by low diagenetic temperature but high 87Sr/86Sr ratios, and high Fe content dolomite mineral. Another is deep burial dolomitization which occured in more strong reducible diagenetic enviornment during late deep burial stage. In general, the degree of dolomitization in burial diagentic enviorment is further enhanced and adjusted. The deep burial dolomite is characterised by high diagenetic temperature and high homogenization temperature of fluid inclusions, but low salinity.