Geochemical Characteristics and Origins of the Lower Cambrian Source Rocks from the Southern Guizhou Depression, SW China
- Publish Date: 2012-08-10
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Key words:
- source rock evaluation /
- marine source rock /
- biomarker /
- productivity /
- anoxic environment /
- Niutitang Formation /
- southern Guizhou Depression /
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Abstract: The Lower Cambrian source rock samples from three typical profiles in the southern Guizhou Depression were analyzed for TOC values, δ13C values, Tmax temperatures, potential generation, and biomarkers using RockEval, GC, GCMS to elucidate the geochemical characteristics and its origin. The results show that the Lower Cambrian black shales in the southern Guizhou Depression are regional marine excellent source rocks with depth of 50150m, and have the TOC values of 0.13%15.40%, average 3.31%(n=169); the kerogens of the source rocks have the δ13C values of 35.79‰-29.88‰, average 32.85‰(n=35), and the kerogen macerals are mainly sapropelinites; the values of the marine vitrinite reflectance of the kerogens are 1.95%3.96%, and the values of the equivalent vitrinite reflectance are 2.02%3.47%; the distribution shapes of the nalkanes are mainly single peak, and the maximum peak carbon are mainly C22, the C30 hopane and C27ααα20R regular sterane are abundant, the regular steranes are mainly C27>C29>C28, the Pr/Ph values are 0.270.62, the source rocks have relative high abundance of gammacerane and dibenzothiophene, the OEP values are 0.821.11,C31 homohopane 22S/(22S+22R) have values of 0.560.63,average 0.59; the source rocks are generally characterized by enrichment in light REE, Ba, Mo, V and U element, relative strong negative anomaly of Ce element , relative strong positive anomaly of Eu element and relative high ratio of U/Th. In summary, the Lower Cambrian marine source rocks in the southern Guizhou Depression have a wide distribution with a thickness of from tens of meters to hundreds of meters, the source rocks have high TOC values, are excellent for organic matter type, and have a postmaturity. It is the product which is jointly controlled by high paleoproductivity and anoxic environment. It can provide abundant organic matter for hydrocarbon generation in the southern Guizhou Depression.
Citation: | Geochemical Characteristics and Origins of the Lower Cambrian Source Rocks from the Southern Guizhou Depression, SW China[J]. Acta Sedimentologica Sinica, 2012, 30(4): 761-769. |