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- W2020160203 abstract "The intraplate Cameros Rift Basin in northern Spain, which has sediments some 6500 m thick, developed between the Late Jurassic and Early Albian. Its facies and their distri- bution in the sedimentary record suggest the basin may contain hydrocarbon systems. The arenite composition of the basin reveals two main petrofacies: (1) a quartzolithic petrofacies, the provenance of which is related to recycling processes that took place in the pre-rift sedimen- tary cover; and (2) a quartzofeldspathic petrofacies mainly related to the erosion of a pluto- nic and metamorphic source of arenite. The succession of these petrofacies reflects two main cycles representing the progressive erosion of their sources, one of 10 Ma, the other of 30 Ma. Such succession is typical of a non-volcanic rift basin. The quartzolithic petrofacies shows early carbonate cements that inhibited compaction and later quartz, feldspar and clay mineral diagene- tic phases. The quartzofeldspathic petrofacies has a rigid framework that maintained the origi- nal pores of the arenite during burial diagenesis. Quartz and K-feldspar overgrowths are common, with secondary porosity occurring as a product of feldspar dissolution. The quartzofelds- pathic petrofacies has a greater potential to act as a hydrocarbon reservoir. This study corroborates the close relationship between the provenance of arenite and its reservoir potential in continental rift basins." @default.
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- W2020160203 date "2013-07-10" @default.
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- W2020160203 title "The influence of the provenance of arenite on its diagenesis in the Cameros Rift Basin (Spain)" @default.
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- W2020160203 doi "https://doi.org/10.1144/sp386.12" @default.
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