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151.
The storage spaces within deeply buried Ordovician paleokarst reservoirs in the Tarim Basin are mostly secondary and characterized by strong heterogeneity and some degree of anisotropy. The types of fluids that fill the spaces within these reservoirs are of great importance for hydrocarbon exploration and exploitation. However, fluid identification from seismic data is often controversial in this area because the seismic velocity for this particular reservoir could be significantly influenced by many factors, including pore shapes, porosity, fluid types, and mineral contents. In this study, we employ the differential effective medium‐Gassmann rock physics model to interpret and discuss the characteristics of conventional karstic carbonate reservoirs in the Tarim Basin that are filled with different fluids (oil, gas, and water) using logging data and thus objectively build corresponding fluid identification criteria. These criteria are subsequently evaluated by amplitude versus offset (AVO) forward analysis based on typical logging data and further applied to ascertain the reservoir fluid types in two different areas in the Tarim Basin based on prestack inversion results. For conventional carbonate reservoirs, gas can be distinguished from heavy oil and water, but heavy oil and water are broadly similar on seismic data. For condensate carbonate reservoirs, water can be differentiated from light oil (i.e., condensates) and gas, but light oil and gas demonstrate substantial similarities in terms of their seismic responses. The predicted fluid results are in good agreement with the results of drilling and oil testing. In particular, modeling the seismically resolvable reservoirs in the carbonate strata in the Tarim Basin, which have needle‐ and sphere‐shaped storage spaces (pore aspect ratio > 0.3) and clay content that is lower than 5%, indicates that fluid properties could be properly evaluated if the porosity is larger than 5% for conventional carbonate reservoirs and >7% for condensate carbonate reservoirs. 相似文献
152.
Mikael Fauvelle Erin M. Smith Sean H. Brown Matthew R. Des Lauriers 《Journal of archaeological science》2012
The design of a projectile delivery system often plays a critical role in the durability and breakage patterns associated with spent projectile points. This paper presents the results of an experimental project designed to examine projectile point durability and breakage patterns between three different hafting methods. Specifically, we compare two asphaltum hafting techniques drawn from archaeological and ethnohistoric accounts from the Central Valley of California with a more stereotypical cross-hatched sinew hafting system. Our results suggest a small yet statistically significant increase in durability among asphaltum hafted points, opening the door to future research on these ethnohistorically documented hafting techniques. 相似文献
153.
当前旅游业和活动会展业的边界逐渐融合,已经进入\"节、会、展、演、赛\"与\"游\"融合发展的大旅游时代。目前国内外对于大型活动与旅游业的互动效应还未作深入研究,文章先从品牌互动、服务互动、客源互动、资源互动四方面提出大型活动与旅游业的互动效应,进而借助化学的\"触媒效应\"和生物学的\"母体效应\"理论,创新性地剖析了二者互动效应的内在机理,并重点对二者互动发展的路径进行了探索,认为理顺管理体制、明晰运行机制,并科学发展\"大型活动旅游\"是准确把握二者互动发展路径的关键。 相似文献
154.
The origin of large‐scale ancient dolomite is one of the most hotly debated topics in sedimentology. The Loushanguan group of the upper 3rd‐Furongian Cambrian series on the south‐eastern margin of the Sichuan Basin consists of numerous dolomites, and the origins of these dolomites have never been reported previously although they are probably good hydrocarbon reservoirs. Based on a systematic analysis of petrology, fluid inclusions, carbon and oxygen isotopes, trace elements and rare earth elements (REEs), this study provides some unique insights into the origins of the dolomites. Four dolomite types have been identified in the study area: dolomicrite, fabric‐retentive oolitic dolomite, fabric‐obliterative dolomite and saddle dolomite cement. In the dolomicrite and fabric‐retentive oolitic dolomite, high Sr contents (with respect to the fabric‐obliterative dolomite) and the lack of two‐phase aqueous inclusions suggest that they formed at shallow‐to‐intermediate burial depths at low temperatures (<50–60°C). Carbon and oxygen isotopes and seawater‐like REE+Y characteristics of the dolomicrite and fabric‐retentive oolitic dolomite indicate that the dolomitizing fluids were evaporated seawater or slightly modified seawater. The obliteration of the original sedimentary fabric and relatively low δ18O and Sr values compared to the fabric‐retentive dolomite indicate that fabric‐obliterative dolomite formed at intermediate‐to‐deep burial diagenesis. The chemical composition approaches pure dolomite and the REE+Y characteristics are similar to those of the fabric‐retentive dolomite, indicating that the fabric‐obliterative dolomite was formed due to the recrystallization of the previously formed fabric‐retentive dolomite at elevated burial depths and temperatures. High fluid inclusion homogenization temperatures (115–150°C), low δ18O values, nonplanar‐a crystals and seawater‐like REE+Y characteristics suggest that saddle dolomite cement formed by reprecipitation of dolomite that related to seawater‐driven and deep burial fluid. In the study area, dolomicrite and fabric‐retentive oolitic dolomite may have been formed by penecontemporaneous or seepage‐reflux dolomitization during early‐stage diagenesis. Subsequently, during progressive burial, most of the fabric‐retentive dolomite was converted into fabric‐obliterative dolomite by recrystallization. This study confirms that fabric‐obliterative dolomite was the main dolomite type, and although deeply buried, these Cambrian dolomites most likely have preserved coeval seawater geochemical signals. 相似文献
155.
Half of the topseals to the world's largest oilfields are evaporites. Rock salt has a thermal conductivity two to four times greater than that of other sedimentary rocks found in oil‐ and gas‐bearing basins. Strong heat conduction through evaporites can increase the geothermal gradient above evaporite deposits, resulting in a positive thermal anomaly and above‐average temperature while simultaneously decreasing the geothermal gradient below evaporites, resulting in a negative thermal anomaly. Most Triassic–Jurassic hydrocarbon source rocks in the Kuqa Basin, western China, are overlain by ~1500‐m‐thick Tertiary evaporites with underlying Cretaceous sandstones and mudstones. Directly measured strata temperatures indicate an obvious break in the steepness of the geothermal gradient above and below Paleogene evaporites, with a significantly steeper geothermal gradient above the evaporites. Simulations of the thermal evolution of source rocks based on data collected from well Kela‐2 indicate that if the thickness of evaporites (mainly rock salt and anhydrite rock) in overlying rocks above source rocks increases compared with the thickness of siliciclastic rocks in the overlying rocks, then strata temperatures and vitrinite reflectance in Jurassic source rocks will decrease accordingly. Our thermal simulations based on the thickness and thermal conductivity of evaporites accurately coincide with previous studies based on homogenization temperatures, hydrocarbon–water contact retrospection, and carbon isotope results from natural gases. The gas generation center located in the Kalasu Tectonic Belt today is also sealed in an evaporite‐related structural trap that formed at this time. Therefore, the speculated natural gas generation times not only correlate with the evaporite‐related structural trap formation, but the calculated maturity of deep source rocks below the evaporites also coincides with current gas reserves. And our studies can help to find the deep oils and gases under thick evaporites. 相似文献
156.
World‐class unconformity‐related U deposits in the Athabasca Basin (Saskatchewan, Canada) are generally located within or near fault zones that intersect the unconformity between the Athabasca Group sedimentary basin rocks and underlying metamorphic basement rocks. Two distinct subtypes of unconformity‐related uranium deposits have been identified: those hosted primarily in the Athabasca Group sandstones (sediment‐hosted) and those hosted primarily in the underlying basement rocks (basement‐hosted). Although significant research on these deposits has been carried out, certain aspects of their formation are still under discussion, one of the main issues being the fluid flow mechanisms responsible for uranium mineralization. The intriguing feature of this problem is that sediment‐hosted and basement‐hosted deposits are characterized by oppositely directed vectors of fluid flow via associated fault zones. Sediment‐hosted deposits formed via upward flow of basement fluids, basement‐hosted deposits via downward flow of basinal fluids. We have hypothesized that such flow patterns are indicative of the fluid flow self‐organization in fault‐bounded thermal convection (Transport in Porous Media, 110, 2015, 25). To explore this hypothesis, we constructed a simplified hydrogeologic model with fault‐bounded thermal convection of fluids in the faulted basement linked with fluid circulation in the overlying fault‐free sandstone horizon. Based on this model, a series of numerical experiments was carried out to simulate the hypothesized fluid flow patterns. The results obtained are in reasonable agreement with the concept of fault‐bounded convection cells as an explanation of focused upflow and downflow across the basement/sandstone unconformity. We then discuss application of the model to another debated problem, the uranium source for the ore‐forming basinal brines. 相似文献
157.
In the Schleswig–Holstein region (S–H) of Germany, most observed near-surface saline ground waters originate from dissolution of shallow salt domes. Previous numerical simulations of thermohaline flow clarified the major mechanisms controlling large-scale density-driven flow. It has been found that, in addition to topographically driven flow, gravitational and thermohaline convection are the primary mechanisms for extensive solute exchange between shallow and deep aquifers. Geological features such as glacial channels control recharge/discharge processes at the surface. Here we address several previously unresolved issues: (i) the impact of a permeable unit (transition zone) between the salt and adjacent units; (ii) the role of variable brine viscosity in affecting regional- (i.e. km-) scale heat and mass patterns; and (iii) the influence of anthropogenic activities such as pumping stations on density-driven flow. We found that geophysical factors play a major role in determining the dynamics of fluid processes. The transition zone significantly influences the flow field and the distribution of heat, slowing the formation of highly concentrated salty plumes. The impact of variable fluid viscosity on the coupled heat and brine flow is twofold. In a colder and highly concentrated environment, such as a shallow salt-dome crest, it retards brine flow. In a less saline environment, variable fluid viscosity enhances thermally induced upward fluid flow. Groundwater extraction from production wells only affects brine and heat flow locally within the upper aquifers. 相似文献
158.
Robert L. Kelly 《Journal of World Prehistory》1997,11(1):1-49
Late Holocene Great Basin prehistory is a spatial and temporal mosaic of lifeways related to changing physical and social environments. Evidence shows changes in technology, subsistence, foraging tactics, and population density, though the causes of these changes are still under investigation. Current research has emphasized the role of wetlands and, related to this, the so-called Numic expansion, whose timing and nature are still poorly understood. Behavioral ecology applied to a macroregional scale probably offers the most useful approach to solving this and other issues, given the exigencies of hunter-gatherer archaeology in a desert environment. 相似文献
159.
A distinctive red-on-buff pottery, found throughout central and southern Arizona, is a hallmark of prehistoric Hohokam culture. To manufacture it, Hohokam potters used a complicated recipe and controls for firing to chemically manipulate their clay and produce a light-colored fabric on which to paint their red designs. In this study, firing experiments and ceramic analysis are used in conjunction with excavation evidence to evaluate competing ideas about the buff ware manufacturing process, investigate where the pots were made, and model the developmental history of red-on-buff production. 相似文献
160.
Audax Z. P. Mabulla 《African Archaeological Review》2007,24(1-2):15-33
In this paper I document the history of hunting and foraging in the Eyasi Basin, northern Tanzania, from about 130,000 bp
to contemporary times, by reviewing the available archaeological, palaeontological, historical and ethnographic data. The
review reveals a complex co-existence and interactions between hunter-foragers and herders and farmers from about 3,000 bp
until the present. In addition, the review exposes intricate opportunities and at the same time risks/constraints that face
extant Hadzabe hunter-foragers in the 21st century. The Hadzabe are a group of about 800–1,000 people who live in the Eyasi
Basin. Traditionally, they are viewed as hunter-foragers—people who acquire nearly all of their food by hunting wild animals
and foraging wild plant foods and honey. Although Hadzabe have been closely surrounded by other ethnic and cultural groups
with whom they have interacted, for at least the last 100 years, their existence as a cultural group in the 21st century is
in doubt. Mitigation measures are required in order to enhance the existence of this important cultural group.
Résumé Cet article est une présentation de l’histoire de chasse et d’affourragement au Bassin Eyasi dans le nord de la Tanzanie, dès les environs de 130.000 ans avant présent, aux périodes contemporaines. On fait une revue des données archéologiques, anthropologiques, paléonthologiques, historiques ainsi que éthnographiques disponibles. La revue indique qu’il y a une coexistence et interaction complexes entre les chasseurs-fourrageurs, bouviers, et cultivateurs il y a 3.000 ans jusqu’au présent. En outre, la revue présente des occasions et en même temps des risques et contraintes complexes qui se posent aux Hadzabé: un groupe d’environ 800–1000 personnes (chasseurs-fourrageurs) qui vivent dans le bassin Eyassi. Traditionnellement, les Hadzabé sont regardés comme, les personnes qui obtiennent présque toutes leurs nourritures de la chair des animaux sauvages, des aliments végétaux sauvage et du miel. Bien que les Hadzabé aient été étroitement environnés et qu’ils aient interagis avec d’autres groupes éthniques et culturels au cours de 100 années passées leur existence au 20ème siècle en tant que groupe culturel est incertaine. Donc, des mesures sont exigées pour soutenir l’existence de ce groupe culturel important.相似文献