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41.
Organic matter was experimentally extracted by supercritical fluids(CO2 1% isopropanol)from petroleum source rocks of different thermo-maturities at different buried depths in the same stratigraphic unit in the Dongying Basin.The results show that supercritical fluid extraction(SFE)is more effective than Soxhlet extraction(SE),with higher amounts and greater varieties of hydrocarbons and soluble organic matter becoming extractive.The supercritical CO2 extraction is therefore considered more valuable in evaluation of petroleum source rocks and oil resources,particularly those of immature types.  相似文献   
42.
This paper presents the attenuation relations of peak ground acceleration and spectral accelerations for rock and soil sites in the central and eastern United States (CEUS). For the bedrock site condition, 56 pairs of moment magnitude M and epicentral distance R are used to simulate ground motion, and for each pair of M and R, 550 samples of ground motion parameters are generated using a seismological model together with random vibration theory and distribution of extreme values. From the regression analyses of these data, the attenuation relations of ground motion parameters for the bedrock site are established. With the aid of appropriate site coefficients, these attenuation relations are modified for the site categories specified in the 1994 NEHRP Provisions. These attenuation relations are appropriate for the assessment of seismic hazards at far-field rock and soil sites in the CEUS.  相似文献   
43.
邱小平  潘淼 《黄金地质》1997,3(4):29-35
小营盘金矿赋存在稳定的缓倾斜石英脉中,但单纯的白色石英脉仅有微弱矿化,只有经过S懊断层剪切拉张破裂和叠加铁白云石化及硫化物蚀变的石英脉才能成为矿体,金矿体的顶底面常被铁白云石蚀变岩和糜棱岩所包裹,而且部分蚀变岩的金含量也达到工业品位,石英脉与蚀变岩作用构成矿体。因此,早期金成矿作用的时代大致与铁白云蚀变同期,含金铁白云石蚀变岩的δ^13C值平均为-4.13‰,Pb-Pb等时线年龄为2711±238  相似文献   
44.
马瑾指出,应把研究我国地震的思路从以断层为中心转变为以活动块体为中心.张培震等把我国大陆及邻区的活动地块划分为两级:Ⅰ级为活动地块区,有青藏等6个;Ⅱ级为活动地块,有拉萨等20余个.我们试图从块体中心论的思想出发,以Ⅱ级活动地块为框架,分析我国大陆近期成组强震发生的构造和震源机制特征.为保持工作的连续和有可比性,我们仍延续李钦祖等采用的选取资料的方法.由于哈佛大学提供的CMT(矩张量)解1976年仅有少量结果,从1977年起才比较完整,所以,我们从1977年起开始研究.1977~2003年我国的强震(西部M≥7,东部M≥6)大致可划分为9个组.  相似文献   
45.
Introduction As far as the frequency and magnitude are concerned, the earthquakes in the sea area to the east of Shanghai are far more strong than in land area with the largest one in the sea area near the Yangtze River mouth being MS=436, while in land, only MS=434 occurred on Sept. 1, 1624. As a moderately strong earthquake active area, the sea area near the Yangtze River mouth, may cause a potential risk to Shanghai. In 1971 and 1996, earthquakes with MS=5~6 occurred in this area. Geo…  相似文献   
46.
Land surface evapotranspiration is an important component both in earth surface heat and water bal-ance, on whose budgets weather and climate depend, to a great extent, for their changes are responsible for the formation and variation of vegetation features on the globe. Besides, the evapotranspiration is an im-portant topic of short-term flood forecasting and the estimation of runoff from mountainous sides. As a result, the problem as to the evapotranspiration has been one of the concerns in …  相似文献   
47.
By shallow seismic prospecting, the Cenozoic Group in the sea area near the Yangtze Rver Mouth can be divided into five seismic sequences. They correspond to the Quaternary,Pliocene, Upper Miocene, Lower Miocene and Eocene respectively. The Quaternary System covers all the detecting area. The Tertiary System overlaps and thins out from NE to SW. The sedimentary basement mainly consists of volcanic rock (J3) and acidic rock (r35). Paleogene or Late Cretaceous basins are not found there. The faults that have been detected are all normal faults. They can be divided into three groups (NE, NW, near EW) by their trend. The NE and NW-trending faults are predominant, and agree with aeromagnetic anomaly. Their length and displacement are larger than that of the EW-trending faults. The activity of the NEtrending faults is different in different segments. The SW segment is a Quaternary fault, the middle segment is a Neogene fault, The NE is Paleogene. But the segment of the NW-trending fault is not obvious. The average vertical displacement rate is about 0.015mm/a.  相似文献   
48.
山西省主要河流流域面雨量预报业务流程   总被引:3,自引:1,他引:3  
以T213、HLAFS模式、MM5中尺度模式输出的格点资料以及日本降水量格点资料为基础,将影响山西降水的天气动力模型归纳为诊断模型,从中引出多个能够全面反映降水模型特征的综合物理因子;根据各种数值模式输出的降水量预报性能和质量优劣特点,依据数值模式的形势场预报优于要素场预报的现实,构造在不同环流形势背景下,启动不同预报方程的面雨量预报业务流程,有效地遏止了在环流形势调整时预报输出不能快速响应的弱点,提高了点和面雨量预报的准确度。  相似文献   
49.
该文针对CAPPS在太原市运行的误差问题,在分析其主要原因的基础上,变换地形背景场,依据不同季节、不同天气形势,在模式中增加对综合误差系数和扬尘系数的调节功能,进行多种数值模拟试验。结果表明:在误差分析基础上确定的模拟试验方案,使主要污染物SO2、NOX和PM10的预报值与监测值的相关系数分别提高到0.96、0.91和0.89,最终使CAPPS成为预报准确率稳定在90%以上的业务化数值模式系统。  相似文献   
50.
The effects of climate change and population growth in recent decades are leading us to consider their combined and potentially extreme consequences, particularly regarding hydrological processes, which can be modeled using a generalized extreme value (GEV) distribution. Most of the GEV models were based on a stationary assumption for hydrological processes, in contrast to the nonstationary reality due to climate change and human activities. In this paper, we present the nonstationary generalized extreme value (NSGEV) distribution and use it to investigate the risk of Niangziguan Springs discharge decreasing to zero. Rather than assuming the location, scale, and shape parameters to be constant as one might do for a stationary GEV distribution analysis, the NSGEV approach can reflect the dynamic processes by defining the GEV parameters as functions of time. Because most of the GEV model is designed to evaluate maxima (e.g. flooding, represented by positive numbers), and spring discharge cessation is a ?minima’, we deduced an NSGEV model for minima by applying opposite numbers, i.e. negative instead of positive numbers. The results of the model application to Niangziguan Springs showed that the probability of zero discharge at Niangziguan Springs will be 1/80 in 2025, and 1/10 in 2030. After 2025, the rate of decrease in spring discharge will accelerate, and the probability that Niangziguan Springs will cease flowing will dramatically increase. The NSGEV model is a robust method for analysing karst spring discharge. Copyright © 2013 John Wiley & Sons, Ltd.  相似文献   
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