scholarly journals Geochemistry of impurity elements of Upper Jurassic deposits of Kazan fields group

Author(s):  
Ksenia Gabova ◽  
Grigorii Kravchenko
Author(s):  
D. A. Petrochenkov

Fossils of marine reptiles are a new jewelry and ornamental material and collected in the Ulyanovsk region from the Upper Jurassic deposits. They consist of (wt. %): calcite — 52, apatite — 24 and pyrite — 23, and also gypsum presents. The contents of radioactive and carcinogenic elements are close to background. The original bone structure of reptiles is preserved. Apatite replaces the bone tissue of marine reptiles, forming a cellular framework. According to the chemical composition, apatite refers to fluorohydroxyapatite with an increased Sr content. The size of the crystals is finely-dispersed. Calcite and pyrite fill the central parts of the cells. Calcite crystals of isometric and elongated shape, 0,01—0,05 mm in size, form blocks up to 0,3 mm during intergrowth. Calcite fills thin, discontinuous veins along the contour of cells with a width of up to 0,03 mm. In calcite, among the impurity elements, there are (wt. %, on the average): Mg — 0,30, Mn — 0,39 and Fe — 0,96. Pyrite forms a dispersed impregnation in calcite and apatite, content of impurities is, wt. %: Ni — up to 0,96 and Cu — up to 0,24. On technological and decorative characteristics of fossils of sea reptiles of Ulyanovsk region are qualitative jewelry and ornamental materials of biomineral group, allowing to make a wide assortment of jewelry and souvenir products.


Author(s):  
Aleksey Yu. Popov ◽  

A comparative analysis of lithogeochemical features of Upper Jurassic rock composition of the lower reaches of the Anabar river and the Urdyukh-Haya cape (Nordvik peninsula) was performed. Several common features, differences and regularities of changes in the section of lithogeochemical characteristics of the studied strata were revealed. The rocks of the Kimmeridgian and upper-middle Volgian have the greatest differences from the higher and lower layers. They are characterized by an increase in the content some of impurity elements (Co, Ni, Zn, U, and some TR). The identified features can be used for correlation when comparing faunal mute strata in the considered part of the sedimentary basin.


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