The oil geology feature of Vienna Basin was summarized and potential of exploration was discussed by analysising the strata of Vienna Basin and fracture development characteristics. Vienna Basin is a pull-apart basin located between the East Alps and West Carpathian. Its basement is composed of the Hercynian Bohemian Massif and Paleozoic and Mesozoic strata. The tectonic evolution can be divided into three stages, including Jurassic extensional rifting, Cretaceous-Early Miocene over-thrusting and Middle Miocene pull-parting stage. There are three structural lays from top to bottom, Jurassic-Cretaceous autochthonous, Permian-Paleogene allochthonous Alpine nappes and Neogene sediments. There are two sets of source rocks: the upper Jurassic marls and Paleogene shale, among which, the Upper Jurassic Kimmeridgian Malmian marls are considered to be the major source rocks. Reservoirs occur at various horizons from Triassic to Neogene Miocene strata, among which, the most important reservoirs are Miocene sandstones that deposit in shallow-water delta environment and contain 76% of all reserves, and the minor reservoirs are the Triassic dolosparite. Neogene shales provide the regional top-seal. After evaluation, it is considered that Mesozoic allochthonous napps (flysch turbidite and Triassic dolomite) and Mesozoic autochthonous succession (the second and the third structural layer) are the most prospective for exploration.

Watermarking algorithms in the H.264/AVC bit-stream are more efficient, but the propagation error introduced would decrease the visual quality severely. In order to reduce the computation complexity of compensation, a new error compensation method is proposed, in which the watermark is embedded into the quantized DCT coefficients and the propagation error gained by a low complexity error prediction module are compensated adaptively. The simulation results show that with the proposed compensation method, a real time video watermarking can be realized, with the features of low complexity, high PSNR and less bitrate increase.

The volcanic rocks of the Yingcheng formation in the Songliao Basin were formed by multiple and intermittent eruptions. Based on the core drilling data, the high-resolution volcanic cycles of the first member of Yingcheng formation in Xujiaweizi fault depression were divided, the volcanic cycle model were built, and the well logging characteristics of different lithology and lithofacies were summarized. The results reveal that, the first member of Yingcheng formation could be divided into 3 volcanic cycles, from the top to the bottom of each cycle, the values of gamma-ray and resistivity were higher and higher, the amplitude and frequency of the well logs in the interface of different cycles changed greatly, indicating the existence of the weathering crust or the sedimentary layer. Logging data of gamma-ray, resistivity and density were considered to be more sensitive in recognition of different volcanic lithology and lithofacies.