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431.
断层圈闭是斜坡区重要的构造圈闭类型,为了识别斜坡区断层圈闭发育部位及其形成时期,基于断层生长机制,分析斜坡区顺向断层圈闭和反向断层圈闭形成演化过程。结果表明:顺向断层圈闭形成于断层"硬连接"阶段,发育在断层下降盘分段生长部位;反向断层圈闭形成于断层开始活动时期,发育在断层上升盘位移最大部位。在此基础上,充分利用详细三维地震资料,结合断距-距离曲线、相干体切片、断层分段生长时期定量表征以及断距回剥等技术,建立了斜坡区断层圈闭发育部位及形成时期的识别方法,并将该方法应用于冀中坳陷文安斜坡典型断层圈闭发育部位及形成时期的识别,研究结果与实际油气分布吻合关系较好。 相似文献
432.
ASTER多光谱遥感数据目前可以用于岩石矿物资源信息的识别和提取。本研究尝试利用ASTER 可见光近红外(VNIR)和短波红外(SWIR)的多光谱遥感数据提取干旱地区的岩石与矿物信息。基于新疆天山西南缘柯坪隆起东部不同地层单元岩石的化学组成和矿物成份以及VNIR SWIR谱域光谱吸收特征的分析,我们采用相关吸收波段深度(RBD)和波段比值(BR)方法对研究区的多光谱遥感数据进行图像处理,有效区分和识别了白云岩、石灰岩、砂岩以及阿克苏群的蓝片岩—绿片岩和砂质片岩。白云岩的CO2-3吸收谱带中心波长位于232〖KG*3〗μm,与灰岩的CO2-3 吸收谱带中心波长位置235 μm相比,具有向短波长方向移动的特点,据此可以利用RBD7、RBD8分别有效的识别白云岩和灰岩; 长英质岩石显示Al OH和Fe3+ VNIR SWIR吸收特征,而基性 超基性岩石显示Fe2+ 和Fe、Mg OH特征,利用不同的铁价态和次要矿物可以区分它们:ASTER band2/band1代表了含Fe3+ 矿物分布信息、ASTER band5/band4代表了含Fe2+ 矿物分布信息、RBD6可以估计Al OH矿物的丰度; 砂质/泥质片岩含较多的多硅白云母、绿泥石、黑硬绿泥石以及风化后表面覆盖的其它粘土矿物,在221 μm(band 6)存在有特征的吸收谱带,并且在165 μm(band 4)具有较高的反射率,而蓝片/绿片岩在221 μm(band 6)反射率较高,不具有明显特征吸收谱带,同时其在165 μm(band 4)反射率较低,因此蓝片/绿片岩ASTER band4/band6 比值低。应用ASTER band4/band6波段比值可以有效的区分开砂质/泥质片岩与蓝片岩/绿片岩。 相似文献
433.
川西什邡地区隐伏断层活动性及其对流体的控制作用 总被引:1,自引:1,他引:0
利用遥感地质解译、土壤微量元素分析、土壤氡气测量以及野外露头观察等手段,在什邡湔氐地区识别出22条隐伏断层。它们按走向可分为北北西向、北东东向和近东西向3组。受关口断层推覆上升的影响,隐伏断层普遍具张扭性,活性较好,含水破碎带发育。从油气水文地球化学和地下水的活动规律来探讨该区断裂和盖层、地下水的配置关系,认为本区油气保存条件总体较差,但在单斜带局部区域寻找水动力圈闭气藏以及在云西—徐家场鼻状背斜上勘探深层气藏仍然有一定的潜力。 相似文献
434.
435.
Vertical profiles of aeolian sand mass flux 总被引:5,自引:0,他引:5
Vertical profiles of the horizontal mass flux of blown sand are investigated experimentally using a passive vertical array in a wind tunnel. Considering lower sampling efficiency of the sand trap in the near-bed region, this investigation is complemented by the measurements of the longitudinal profiles of mass flux made using a horizontal sand trap. The experiments were conducted with two test sands and five different stream velocities.In the upper part of the vertical profile, the measured data exhibit an exponential decay distribution with a positive deviation occurring in the near-bed region. The measured longitudinal profiles are similar to the measured vertical profiles. Linking both profiles and the modes of sand transport, it is possible that saltating sand grains give rise to the well-known exponential decay distribution of mass flux, and that creeping and reptating grains force a deviation from it. A simple equation applicable for both the vertical and the longitudinal sand mass flux variations is introduced and the parameters are estimated from experimental data. 相似文献
436.
A total of 6085 adult Trichoptera (excluding Hydroptilidae) representing 12 families, 31 genera, and 56 species were collected by a combination of Malaise net and light trapping from July 1998 to July 1999 at three hill‐country sites of contrasting catchment land use (100% native forest, a pasture site with native forest headwaters, and 100% pasture) in the Waikato, northern New Zealand. Forty‐eight species of Trichoptera were collected from Malaise nets and 45 species from light traps. Eleven species of Trichoptera were only ever collected from the Malaise nets and seven species from only the light traps. At the native forest site, Malaise nets collected more species and taxa of conservation interest than did light traps, possibly reflecting diurnal activity or non‐attraction to light by some species. Several species of Trichoptera showed site specificity and most of these were found at the native forest site. Twenty‐eight species were active for at least 6 months of the year with at least four species active all year. A minimum overnight air temperature of at least 9°C was required to induce Trichoptera flight activity, but large‐scale flight activity may require temperatures greater than 14°C. Trichoptera with free‐living and net spinning larvae exhibited extended flight periods, and for three species examined there were bi‐modal activity peaks. Adult caddisflies with cased larvae which grazed on epilithic food resources generally had reduced flight periods and one species had a well‐defined, synchronous periodicity. These findings suggest flight periodicity may partly be a functional response to larval food availability. 相似文献
437.
The California spiny or red rock lobster, Panulirus interruptus, is an ecologically and economically important species that has been exploited since the 1800s. No previous study in California has assessed the impacts of the recreational or commercial lobster harvest. Before the 2003–04 commercial and recreational lobster seasons, we conducted a fishery‐independent trap survey at Santa Catalina Island to document the impact of the lobster fisheries on the size structure, abundance, and sex ratios of mature P. interruptus (>65 mm carapace length (CL)). We concurrently sampled a predominantly commercially fished area, a recreationally fished area, and a 23‐year‐old invertebrate no‐take (INT) reserve. Relative to the INT reserve, legal‐size lobsters in the recreational area were similar in CL, but 31% less abundant. Legal‐size lobsters in the commercial area were 8% smaller and 70% less abundant than those in the INT reserve. The sex ratio of legal‐size lobsters, although near 50:50 in the recreational and INT reserve areas, was male‐dominated (67:33) in the commercial area. Differences in CPUE and mean CL of sub‐legal lobsters in the recreational and commercial areas suggest that factors in addition to harvesting pressure may affect these populations. Total biomass of mature lobsters in the recreational and commercial areas was 92% and 45%, respectively, of biomass in the INT reserve. Fecundity in the recreational and commercial areas was 83% and 42%, respectively, of fecundity in the INT reserve. This study provides preliminary data for future ecological studies and fisheries management evaluations. 相似文献
438.
河北霸县凹陷兴隆宫地区沙三段岩性油气藏成藏条件与圈闭模式 总被引:2,自引:2,他引:0
裂谷型凹陷深层的油气勘探前景一直为众多学者所关注。兴隆宫地区紧临霸县生油洼槽,其沙三段埋深较大,勘探程度较低,少量探井证实这一些地区的沙三段具良好的油气成藏前景。应用石油地质学中的油气成藏理论,系统论述该区有利的岩性油气藏成藏条件与圈闭模式:沙三段圈闭接近沙四段、沙三段及沙一段的油源,具有优越的油气源条件;沙三段大型三角洲前缘与浊积扇等储层条件较好;沙三段同沉积构造与坡折带利于岩性油气藏形成;膏泥岩、盐岩及泥岩提供盖层与保存条件。而该区沙三段岩性油气藏成藏的圈闭模式可分为3个区带:陡坡带主要发育构造—岩性圈闭、小型三角洲前缘砂岩岩性圈闭;缓坡带以大型三角洲前缘砂岩岩性圈闭、地层超覆、地层不整合圈闭为主;而洼槽带以坡折附近的尖灭砂体圈闭为主。陡坡坡折之下发育扇三角洲前缘与浊积扇圈闭;缓坡坡折之下发育与低位三角洲、浊积扇及滩坝砂体有关的岩性圈闭。通过研究可以确定东部文安缓坡坡折带以下地区是目前岩性油气藏的最有利勘探区带。 相似文献
439.
从松辽盆地的构造反转看中国东部盆地构造圈闭的形成 总被引:6,自引:0,他引:6
通过对松辽盆地构造反转的分析,把该盆地构造反划分为3种类型:平面上分为4个反转向构造带,结合中国东部含油气盆地构造样式和演化机制,认为松辽盆地的构造反转不同局部现象,它代表了中国东部裂谷盆地演化的普遍模式,并与构造圈闭,油气藏的形成密切相关,中国东部盆地重要的构造反转4期;盆地内众多构造圈闭类型是多种地质应力联合作用和多期构造作用叠加的结果,而后期的挤压反转到了加剧和定型作用,中国东部燕山-喜山期 相似文献
440.
Settling particles play an important role in transporting organic carbon from the surface to the deep ocean. It is known that major components of settling particles are biogenic silicates (opal), biogenic carbonate (CaCO3), lithogenic clays and organic matter. Since each component aggregates and/or takes in organic carbon, all of these components have the ability to transport particulate organic carbon (POC) to the interior of the ocean. In this study, sediment trap experiments were carried out in four areas of the western North Pacific (including a marginal sea). Factors are proposed that correlate the composition of settling particles with POC flux. Annual mean organic carbon fluxes at 1 km depth in the western North Pacific Basin, Japan Sea, Hidaka Basin and northern Japan Trench were found to be 14.9, 18.1, 13.0 and 6.6 mg/m2/day, respectively. Organic carbon flux in the western North Pacific was greater than that in the Eastern North Pacific (7.4), the Equatorial Pacific (4.2), the Southern Ocean (5.8) and the Eastern North Atlantic (1.8). In the western North Pacific, it was calculated that 52% of POC was carried by opal particles. Opal is known to be a major component even in the Eastern North Pacific and the Southern Ocean, and the opal fluxes in these areas are similar to those in the western North Pacific. However, the organic carbon flux that was carried by opal particles (OCopalflux) in the western North Pacific was greater than that in the Eastern North Pacific and the Southern Ocean. These results indicate that the ability of opal particles to transport POC to the deep ocean in the western North Pacific is greater than that in the other areas. 相似文献