2008年大柴旦M_w6.3级地震的InSAR同震形变观测及断层参数反演

2008年11月10日,青海省大柴旦地区发生了Mw6.3级地震。本文利用EnviSat卫星升降轨SAR数据和差分干涉测量技术提取了同震形变场,基于均匀位错模型反演确定了地震断层参数,然后利用格网迭代搜索法确定了较优断层倾角,同时基于非均匀位错模型获得了精细滑动分布。结果表明,地震使得上盘区域沿降轨、升轨视线向分别产生最大约8.5cm、10cm的抬升;较优断层倾角为47.9°;地震滑动未延伸至地表,主要发生在地下8.2~23.7km深度范围内,最大和平均滑动量为0.5m和0.19m,平均滑动角为104.9°。反演的地震矩为3.74×1018 N·m,矩震级为Mw6.35。     

琼东南盆地华光凹陷天然气水合物稳定带厚度的影响因素

为了探讨琼东南盆地华光凹陷海底天然气水合物稳定带的分布规律,定量研究了静水压力、底水温度、地温梯度和气源组分对水合物稳定带的影响程度。在此基础上,分析了华光凹陷现今甲烷水合物稳定带的厚度分布。最后,综合各因素的历史演化过程,初步探讨了华光凹陷1.05 Ma BP以来天然气水合物稳定带的演化。结果表明:(1)气源组分和海底温度的变化对研究区内水合物稳定带的影响较大;水合物稳定带厚度与海底温度呈良好的线性负相关性。(2)水深超过600 m的海域具备形成天然气水合物的温压条件;超过600 m水深的海域水合物稳定带厚度大部分超过 100 m,其中西北部稳定带的最大厚度超过300 m,是有利的水合物勘探区。(3)华光凹陷1.05 Ma BP以来天然气水合物稳定带厚度经历了快速增厚–窄幅变化–快速减薄和恢复的过程。麻坑群与水合物稳定变化敏感区在空间上具有较好的叠合关系。结合前人的研究成果,推测其形成与天然气水合物的分解释放有关。     

区域矿产资源经济研究的发展趋势及值得注意的若干问题

区域矿产资源经济研究的发展趋势是：区域矿产资源经济研究与人口、环境科学汇流,更加注重应用研究,研究目标的多元化,研究地域的扩大化,研究方法的现代化．值得重视的几个问题有：区域矿产资源可持续发展问题;区域矿产资源合理有效利用的客观标准;区域矿产资源的经济和人口承载能力;计算机技术的应用;人工神经网络等现代科学技术的应用;区域矿产资源资产评估的理论与方法;区域矿产资源经济研究模型系统的开发等．     

Single Nucleotide Polymorphism of FSHβ Gene Associated with Reproductive Traits in Japanese Flounder (Paralichthys olivaceus)

Follicle stimulating hormone β (FSHβ) of Japanese flounder (Paralichthys olivaceus) plays a key role in the regulation of gonadal development.This study aimed to investigate molecular genetic characteristics of the FSHβ gene and elucidate the effects of single nucleotide polymorphisms (SNPs) of FSHβ on reproductive traits in Japanese flounder.We used polymerase chain reaction single-strand conformation polymorphism (PCR-SSCP) and sequencing of the FSHβ gene in 60 individuals.We identified only an SNP (T/C) in the coding region of exon3 of FSHβ.The SNP (T/C) did not lead to amino acid changes at the position 340 bp of FSHβ gene.Statistical analysis showed that the SNP was significantly associated with testosterone (T) level and gonadosomatic index (GSI) (P0.05).Individuals with genotype TC of the SNP had significantly higher serum T levels and GSI (P0.05) than that of genotype CC.Therefore, FSHβ gene could be a useful molecular marker in selection for prominent reproductive trait in Japanese Flounder.     

鲢鳙对浮游动物群落结构的影响

1990年4—7月,在武汉东湖运用围圈的方法,研究了鲢(Hypophthalmichthys molitriac)、鳙(Aristichthys nobilis)对浮游动物群落结构的影响。观察表明:在鲢鳙混养的围圈中,原生动物和小型轮虫的数量较多,而甲壳动物和大型轮虫较少。在无鱼的围圈中,结果正好相反。就浮游动物平均生物量而论,无鱼的两个围圈(55.035mg/L和38.374mg/L)比鲢鳙混养的两个围圈(3.028mg/L和3.490mg/L)高得多。甲壳动物(无节幼体除外)的体长频度分布表明:在无鱼的围圈中,大型甲壳动物的频度比有鱼的围圈高得多。围圈实验表明:鲢鳙的摄食促进了浮游动物向小型化方向发展。     

台湾集集大地震及其余震的长周期地震动特性

用丰富的高质量数字强震记录对台湾集集大地震及余震的长周期地震动特性进行了研究. 本文主要研究了长周期地震动的强度随震级、距离及场地条件的变化情况;同时对近断层的长周期地震动特性进行了分析. 结果表明,集集大地震及余震的长周期地震动反应谱的形状主要受场地条件和震级控制（D+E类场地的反应谱要比B+C类的宽,震级大的反应谱要比震级小的宽）,而受距离影响并不显著;近断层长周期地震动明显受断层活动特性影响:上盘的长周期地震动比下盘的强,北部的比南部的强.      

MCZT在气枪震源信号频谱分析中的应用

气枪震源信号是短时非平稳信号,采用频谱细化算法能提高频谱分析的准确性。首先进行了改进线性调频Z变换(MCZT)和FFT两种频谱分析算法的误差仿真计算,然后进行气枪震源的水下子波信号和地震波信号的对比计算。结果表明MCZT计算误差较小、计算时间较少,能有效提高气枪震源信号频率和幅度特征提取的准确性,是气枪震源信号频谱特征分析的一个有效方法。     

基于居民认知视角的小城镇群网化影响因素分析——以常州市为例

伴随着市场经济的发展,小城镇群网化对区域间要素流动和城乡一体化发展的重要性逐渐显现。利用2011年7月对常州市小城镇镇区常住居民的随机抽样调查数据,对调查样本和居民认知情况进行了统计分析;运用累积Logistic模型,分析了居民认知视角下小城镇群网化发展的影响因素。结果显示:居民出行交通方式、居民月消费水平、保障房制度、产业发展和集贸市场的健全程度5个因素对小城镇群网化发展影响显著,并反映出市民对小城镇群网化发展具有强烈的主观诉求,但促进小城镇群网化发展的政策供给存在不足。最后提出了促进常州市小城镇群网化发展的具体建议。     

Experimental Investigation on Coal Deterioration Deformation Mechanism and Energy Evolution Law after High Temperature Pre-damage

Geotechnical and Geological Engineering - Deep coals are generally in a high geothermal environment, and when UCG (underground coal gasification) is carried out, the long-term high temperature...     

Rock magnetic properties and palaeomagnetic results of sediments from a stone implement layer in the Bose Basin,Guangxi

Directional samples were taken to study rock magnetism and palaeomagnetic records from the Dong- sheng profile, which is 5 m thick and on the northwest edge of the Bose Basin. Mineralogy and rock magnetism of typical samples indicate that coarse granular titanomagnetite, and fine-grained hematite, superparamagnetic maghemite formed by pedogenesis are in the sediment, which has undergone many transformative processes during different stages of pedogenesis. Parallel samples were taken for thermal demagnetization (TH) (0 to 680℃) and alternating field (AF) demagnetization (0 to 80 mT) respectively. Experimental results of these two kinds of demagnetization illustrate that there are two or more magnetic components in the samples. Intensity of NRM decreases by almost 60% to 90% rapidly when the temperature ranges from 100℃ to 350℃, with a steady magnetic component. It is impossible to analyze the magnetic components at high temperature because those fluctuate widely when the temperature is higher than 400℃. Steady magnetic components from 100℃ to 350℃ indicate that the remanence was mainly carried by fine-grained hematite formed by pedogenesis, reflecting a change in the geomagnetic field while the magnetite was being oxidized into hematite by chemical weathering after deposition. The formative age of the sediments cannot be obtained by magnetic methods in this profile.