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311.
312.
通过对沙粒的起动过程以及粒床相互作用机理进行参数化处理,利用计算流体力学方法与离散动力学模拟对风场和沙粒进行耦合迭代,建立了基于欧拉—拉格朗日模式的、适用于研究风沙流二维特征的风沙跃移数值模型。通过模拟沙粒集团以及单颗沙粒跃移运动的随机特征,有效描述了风沙流垂向以及沿程变化规律,并且能够输出任意时刻每颗沙粒的空间位置、速度和加速度等信息。输沙通量的空间分布与现场观测实验数据有较高的吻合度,摩阻风速和风速廓线两个宏观物理量的变化情况与风沙流形成和发展的物理实际相符,说明了本数值模型和计算方法的合理性。 相似文献
313.
Chao Zhang Chang-Qian Ma Qun-An Liao Jin-Yang Zhang Zhen-Bing She 《International Journal of Earth Sciences》2011,100(7):1665-1684
Several major volcanic zones are distributed across the eastern North China Craton, from northwest to southeast: the Greater
Xing’an Range, Jibei-Liaoxi, Xishan, and Songliao Basins, and the Yanji, Huanghua, and Ludong volcanic zones. The Huanghua
depression within the Bohai Bay Basin was filled by middle Late Mesozoic volcanic rocks and abundant Cenozoic alkaline basalts.
Zircon LA-ICP-MS and SHRIMP U–Pb dating show that basic–intermediate volcanic rocks were extruded in the Early Cretaceous of 118.8 ± 1.0 Ma (weighted mean 206Pb/238U age), before Late Cretaceous acid lavas at 71.5 ± 2.6 Ma. An inherited zircon from andesite has a Paleoprotoerozoic core
crystallization age of 2,424 ± 22 Ma (206Pb/207Pb age) indicating that the basement of the Bohai Bay Basin is part of the North China Craton. Early Cretaceous basic and
intermediate lavas are characterized by strong enrichments in LREE and LILE and depletions in HREE and HFSE, indicating a
volcanic arc origin related to oceanic subduction. Depletion in Zr only occurs in basic and intermediate volcanic rocks, while
depletions in Sr and Ti exist only in acid samples, indicating that the acid series is not genetically related to the basic–intermediate
series. Formation ages and geochemical features indicate that the Late Cretaceous acid lavas are products of crustal remelting
in an extensional regime. Combined information from all these volcanic zones shows that subduction-related volcanic rocks
were generated in the Jibei-Liaoxi and Xishan volcanic zones during the Early Jurassic, about 60 Ma earlier than their analogues
extruded in the Huanghua and Ludong volcanic zones during the Early Cretaceous. This younging trend also exists in the youngest
extension-related volcanism in each of these zones: Early Cretaceous asthenosphere-derived alkaline basalts in the northwest
and Late Cretaceous in the southeast. A tectonic model of northwestward subduction and continuous oceanward retreat of the
Paleo-Pacific Plate is proposed to explain the migration pattern of both arc-related and post-subduction extension-related
volcanic rocks. As the subduction zone continuously migrated, active continental margin and backarc regimes successively played
their roles in different parts of North China during the Late Mesozoic (J1–K2). 相似文献
314.
Evaluation of spatial-temporal variability of species composition and diversity in oceanic ecosystems is not easy because it is usually difficult to obtain sufficient data quantifying such variability.In this study,we examined pelagic species diversity indicators,species richness,Shannon-Wiener index of diversity and Hurlbert’s species evenness,for fish assemblages from two areas(north and south) in the North Pacific Ocean(2°±12°N,178°E±165°W) during May±July 2008.The assemblages were based on data collected by an onboard scientific observer during a commercial longline fishing trip.The species richness and Shannon-Wiener diversity index of fish assemblages in the northern area were slightly higher than those in the southern area,although these differences were not significant(t test,P.0.05).Non-parametric multidimensional scaling and analysis of similarities indicated that there were significant differences in fish assemblages between the two areas(P,0.01). 相似文献
315.
浙东南某些中生代侵入岩体的^40Ar—^39Ar年龄测定 总被引:13,自引:3,他引:13
采用~(40)Ar~(39)Ar定年技术测定了浙东南几个侵入于磨石山群中的燕山期中酸性岩侵入体的年龄。梁弄岩体的石英闪长岩和二长花岗岩的年龄为101Ma,龙王堂岩体的花岗岩和钾长花岗岩的年龄均为110Ma,山头郑石英闪长岩年龄为108Ma,洪公石英正长岩的年龄为124Ma。此年龄范围与早白垩世太平洋洋底快速扩张期相当。 相似文献
316.
佘彬彬 《武汉大学学报(信息科学版)》1989,(1)
本文同时顾及地面网尺度系统误差和卫星网尺度系统误差对各自网点坐标的影响,对联合平差中常用的两种7参数转换模型:Bursa模型和Molodensky模型进行了分析比较,在此基础上,提出了一种新的7参数转换模型;建立了甚长基线(VLBI)、卫星网和地面网联合平差的数学模型,并用模拟数据进行了数值分析,得到了一些有益结论。 相似文献
317.
318.
319.
辽宁丹东五龙金矿矿化类型及其构造控制机理 总被引:7,自引:1,他引:7
位于辽宁丹东地区的五龙金矿受NE向剪切系统控制.在剪切带发展演化过程中,于不同阶段形成不同类型的金矿化。在早期韧性剪切带上升剥蚀阶段出现的NE向脆-韧性线状剪切带,控制同剪切带型金矿;叠加在韧性剪切带之上的NNE向一级断裂控制破碎带蚀变岩型金矿的形成和分布;沿SN向和NW向的二级断裂构造控制含金石英脉型金矿。 相似文献
320.
后效严重型强震重复时间讨论 总被引:1,自引:0,他引:1
本文根据中国七个地区的古地震重复时间统计以及某些大震区的低电阻特性,建立了震源热模型并进行了定量计算。给出了后效严重型的大震(M≥7)的重复时间。 相似文献