Geochemical and isotopic composition of organic matter in the Kupferschiefer of the Polish Zechstein basin: relation to maturity and base metal mineralization

Drill core samples from the Kupferschiefer of Poland were collected through out the Zechstein basin. The samples included oxidized Kupferschiefer from Rote Faule zones, adjacent Cu-mineralized Kupferschiefer of southwestern Po land, and drill cores from the central and northern parts of the Zechstein basin. The Kupferschiefer samples reflect differences in base metal mineral ization and in burial depth (630-5067m). The organic matter of the Kupfersc hiefer is characterized by Rock-Eval and GC-MS analyses. Classification of kerogen by hydrogen and oxygen indices (HI, OI), correlations of T-max vs t he present depth of the Kupferschiefer, soluble organic matter (SOM) yields , and relative proportions of saturated and aromatic hydrocarbons of the SO M provide evidence for an oxidative alteration of organic matter in highly mineralized Kupferschiefer samples near the Rote Faule zones. This is confi rmed by differences in the composition of the saturated and aromatic hydroc arbon fractions of the soluble organic matter: Saturated hydrocarbons from Rote Faule samples are dominated by short-chain n-alkanes and higher abunda nces of pristane and phytane relative to heptadecane (n-C17) and octadecane (n-C18), respec tively, compared with samples more distant to the Rote Fau le zone. Compositional changes of the aromatic hydrocarbon fractions with d ecreasing distance to that zone are characterized by the occurrence of poly cyclic aromatic hydrocarbons and elevated ratios of phenanthrene to methylp henanthrenes that are attributed to demethylation reactions and resulted in a decrease of the methylphenanthrene index (MPI 1). Kupferschiefer samples from the barren zone of the Polish Basin do not show these alteration patt erns. The observed variations in organic matter composition with burial dep th are consistent with changes due to increasing thermal maturation. Maturi ty assessment is achieved from MPI 1 and the methyldibenzothiophene ratio ( MDR). From the relationship between the maturity of organic matter in terms of vitrinite reflectance values and depth of the Kupferschiefer strata, a continuous increase in reflectance of vitrinite is obtained within the Poli sh Basin. The alteration pattern of organic matter related to base metal mi neralization of the Kupferschiefer corresponds to changes in the isotopic c omposition of organic carbon and calcite. Kerogen within, or close to, Rote Faule zone is enriched in C-13 caused by the preferential release of isoto pically light organic compounds through progressive degradation of organic matter. The opposite tendency towards lower delta(13)C and delta(18)O value s of calcite provides evidence for isotopic exchange between carbonate and the oxidizing, ore-bearing solutions and for organic matter remineralizatio n. In contrast, organic matter and calcite from the Kupferschiefer do not s how regular trends in delta(13)C with increasing thermal maturation.