黄海南部、东海北部黄鮟鱇的繁殖生物学特性

黄鮟鱇雌鱼初次性成熟体长为293 mm,初次性成熟年龄为1.5龄。繁殖季节为2-5月,以4-5月为盛产期。雌鱼成熟系数在4月达到最大,5月次之,雄鱼成熟系数在5月最大。其绝对繁殖力介于(3.11~14.1)×105粒之间,平均为(6.74±2.87)×105粒,相对繁殖力(F/L)为883~2 153粒/mm,平均为(1 521±581)粒/mm,相对繁殖力(F/W)为181~426粒/g,平均为(264±76)粒/g。对Ⅳ期卵巢132颗卵细胞的直径测定结果显示,卵径范围为1.30~1.76 mm,平均为(1.59±0.19)mm,明显的1个峰值出现在1.575~1.625 mm,占总卵粒数的33.3%,其卵径分布不均匀,应属于一次性产卵类型。     

浙江北部沿岸张网作业区鱼类优势种时空变化研究

根据2007-2009年浙江北部沿岸张网作业区（29°30′～31°00′N、122°00′～123°00′E）进行监测所获得的资料,用相对重要性指数、Margalef物种丰富度指数、Shannon-Wiener多样性指数、Pielou均匀度指数等指标,对浙江北部沿岸张网作业区鱼类的季节变化、时空分布和重要经济种类生物学变化进行分析。结果表明：浙江北部沿岸张网作业区第一、二、三季度共有优势种8种,第四季度优势种7种。将调查的10个作业点划分为5个区域,其中,黄大洋、嵊泗区共出现优势种6种;普陀区和岱衢洋共有优势种5种;杭州湾有优势种3种。对黄龙点主要经济种类生物学测定和分析得出,本次调查主要经济鱼类带鱼、小黄鱼、银鲳等平均体重较历史上有较大变动,群体组成趋于小型化。     

基于谱风险测度的期指保证金水平设定

沪深300股指期货合约已经在2010-04-16正式上市交易.在股指期货合约的交易中,设定合适的保证金水平是风险控制的关键.在能够保证覆盖价格波动的情况下,保证金水平应该尽可能地降低以提高资金使用效率和降低交易成本.基于极值理论的POT模型,利用谱风险测度对沪深300股指期货合约的保证金水平做实证研究,并对比传统的VaR方法和ES方法,实证结果表明,当前的保证金水平设定较高,通过谱风险测度所设定的保证金水平比较合适.     

闽北红色旅游SWOT分析及对策研究

运用SWOT分析法,对福建省闽北地区发展红色旅游的优势、劣势、机会及威胁进行了初步分析,并就发展闽北红色旅游提出了若干对策。     

股指期货市场强行平仓风险估计

考虑了我国指数期货市场投资者被强行平仓风险的计算问题.利用鞅的最优停止理论,给出了一个强行平仓概率和投资者保证金资本存量之间的关系.采用300指数历史数据的研究发现,为了保证一个40 d左右的指数期合约以90%以上的概率不被强行平仓,投资者需要为每份合约准备至少30万人民币的保证金资本;若要维持一个寿命为55 d的指数期货合约,投资者需要为每份合约至少准备50万左右的保证金资本.一个仅有200万保证金资本存量的投资者最多能持有4份寿命为55 d的期货合约.     

粤北牛岱辉绿岩脉的地球化学特征及其成因研究

牛岱辉绿岩脉位于粤北诸广岩体南部.牛岱辉绿岩具有低SiO2 (45.04％ ～48.64％)、高TiO2( 2.02％～ 3.23％)和TFeO含量(17.00％～ 19.80％)、富集K,Rb,Ba等大离子亲石元素和La,Nd,Eu,Tb等稀土元素、Nb-Ta亏损轻微、稀土总量较高(112.1×10-6 ～132.7...     

廊坊北三县地区地面沉降时空分布特征与成因分析

精确、高效的垂向形变监测与分析对地面沉降灾害防控与地球动力学研究均具重要意义。采用永久散射体干涉测量(PS-In SAR)技术获取廊坊北三县地区2007~2010年地面沉降时间序列信息,并结合地层岩性、活动构造、城镇化水平与地下水开采等形变影响因素,分析研究区沉降时空分布特征与成因。结果表明:研究区地面沉降非均匀性显著,且表现出季节性变动特征;厚度较大的冲积、湖积地层沉降较发育,沉降分布受构造控制明显,断层两侧形变速率差异大,局部区域人为诱因占主导;一般、严重沉降区分布与0IBI差值0.4区域具一定空间响应,且在典型区内与中、深层承压水位漏斗空间展布吻合较好,但沉降中心偏西北。     

Timing of the Wudangshan, Yaolinghe volcanic sequences and mafic sills in South Qinling: U-Pb zircon geochronology and tectonic implication

The Wudangshan, Yaolinghe volcanic-sedimentary sequences and doleritic-gabbroic sills comprise the largest exposed Precambrian basement in South Qinling. Zircons separated from 5 volcanic-pyroclastic samples of the Wudangshan Group, 2 volcanic samples of the Yaolinghe Group and one sample for the mafic sills were used for U-Pb dating by laser ablation-inductively coupled plasma mass spectrometry （LA-ICPMS）. The results reveal that the Wudangshan volcanic sequence was formed at （755±3） Ma （a weighted mean from the 5 samples, MSWD=0.47）, whereas the Yaolinghe volcanic suite and the mafic sill were crystallized at （685±5） （2 samples, MSWD=0.36） and （679±3） Ma （MSWD=1.6）, respectively, which are equal to each other within analysis errors. These ages are markedly younger than those previously documented for the rocks. The newly obtained ages for the Wudangshan and Yaolinghe Groups are Identical to those of the bottom Liantuo and slightly older than those of the Nantuo Formations, respectively, lower strata of the Nanhua （middle to late Neoproterozoic） stratotype section in eastern Three Gorges, Yangtze creton. A range of inherited magmatic zircons was recognized with ages of 830 to 780 Ma, which are typical of Neoprotzrozoic magmatisms recorded along the margins and interior of the Yangtze craton. Thus, there is Neoproterozoic basement comprising 830-780 Ma igneous suites in South Qinling; the inherited zircons were detrital sediments derived from the northern margin of the Yangtze craton. Accordingly, it is suggested that the South Qinling is a segment of the Yangtze creton before the Qinling Orogeny.     

Evidence of crustal ＇channel flow＇ in the eastern margin of Tibetan Plateau from MT measurements

Magnetotelluric （MT） survey has been carried out in the eastern margin of the Tibetan Plateau and its neighboring Shimian-Leshan area, Sichuan Province. Analysis of this MT data reveals that the electric structure of the Tibetan Plateau differ much from that of the Sichuan block. In general, the electric resistivity of crust beneath the Sichuan block in the east is larger than that of the eastern margin of the Tibetan Plateau in the west. The crust of the plateau is divided into upper, middle, and lower layers. The middle crust is a low resistivity layer with minimum down to 3-10Ωm about 10-15 km thick. It presumably contains partial melt and/or salt-bearing fluids with low viscosity, prone to deform and flow, producing a ＂channel flow＂ under the southeastward squeeze of the eastern Tibetan Plateau. This low-resistivity layer makes the upper crust decoupled mechanically from the lower crust. In the brittle upper crust, faults are dominated by left-lateral strike-slip and thrust motions, leading to surface rising and shallow earthquakes. The low-resistivity layer also cut the Xianshuihe-Anninghe fault zone into two sections vertically. In this region, the thicknesses of upper, middle, and lower crust vary laterally, producing a transitional zone in the eastern margin of the Tibetan Plateau characterized by thicker crust and higher elevation in the west and thinner crust and lower elevation in the east.     

浙江中北部沿海人工渔礁拟投放区夏季近底层水生游泳动物组成分析

通过对浙江中北部海区13个人工渔礁拟投放点的拖网调查,从而获得了各拟投放点的水生游泳动物组成数据并进行分析,研究结果表明:在浙江中北部人工渔礁拟投放区海域共捕获水生游泳动物50种,分别隶属于3门,3纲,14目,34科。其中,鱼类26种,虾蟹类20种,头足类3种,其他甲壳类1种。各类群的资源重量密度指数和资源尾数密度指数的最大值分别出现在P1号站和P7号站。水生游泳动物的优势种为中国毛虾Acetes chinensis、中华管鞭虾Solenocera crassicor-nis、矛尾鰕虎鱼Chaeturichthys stigmatias、口虾蛄Oratosquilla oratoria、须赤虾Metapenaeopsis barbata、葛氏长臂虾Palaemon gravieri,常见种为双斑蟳Charybdis bimaculata、鹰爪虾Trachypenaeus curvirostris、狼牙鳗鰕虎鱼Taenioides rubicundus、哈氏仿对虾Parapenaeopsis hardwickii、长蛸Octopus variabilis、日本蟳Charybdis japonica、皮氏叫姑鱼Johnius belengerii、带鱼Trichiurus japonicus、前肛鳗Dysomma anguillare、剑尖枪乌贼Loligo edulis、刺鲳Psenopsis anomala、小黄鱼Larimichthys poly-actis、细巧仿对虾Parapenaeopsis tenella等。