1945—1995年国际参考地磁场   总被引：1，自引：0，他引：1  

安振昌 《地球物理学进展》1992,(2)

本文回顾了国际参考地磁场(IGRF)的建立和修改过程;介绍了最新的IGRF模型,即第六代国际参考地磁场;综述了国际参考地磁场在地磁学中的应用,并指出了在使用过程中需要注意的一些问题.  相似文献   

1950-1980年中国地区主磁场模型的建立及分析   总被引：3，自引：10，他引：3  

安振昌  徐元芳 《地球物理学报》1991,34(5):585-593

本文根据丰富的地磁资料,用泰勒多项式方法推算出1950.0、1960.0、1970.0和1980.0年中国地区的主磁场模型,绘制出各个年代地磁要素的等值线图,分析研究了局部地区地磁场泰勒多项式模型的特点.  相似文献   

滇西高黎贡断裂带糜棱岩的显微变形特征及其构造意义   总被引：3，自引：2，他引：3  

李康  钟大赉 《岩石学报》1991,7(3):65-72,T001

采用扫描电镜(SEM)、超高压透射电镜(HTEM)及电子探针等手段研究了主高黎贡断裂带糜棱岩的显微构造特征,提出长石经历了碎粒流动和部分固态塑性流变过程;而石英晶粒经历了动态重结晶和静态回复阶段。认为高黎贡剪切带是在相当于高绿片岩相—低角闪岩相的变质条件下形成的,是晚第三纪右旋走滑活动的产物。  相似文献   

Fabric controls on strain accommodation in naturally deformed mylonites: The influence of interconnected micaceous layers     

《Journal of Structural Geology》2016

We present microstructural analyses demonstrating how the geometrical distribution and interconnectivity of mica influences quartz crystallographic preferred orientation (CPO) development in naturally deformed rocks. We use a polymineralic (Qtz + Pl + Kfs + Bt + Ms ± Grt ± Tur) mylonite from the Zanskar Shear Zone, a section of the South Tibetan Detachment (NW Himalaya), to demonstrate how quartz CPO intensity decreases from quartz-dominated domains to micaceous domains, independently of whether or not quartz grains are pinned by mica grains. We then use a bimineralic (Qtz + Ms) mylonite from the Main Central Thrust (NW Himalaya) to show how increasing mica grain connectivity is concomitant with a systematic weakening of quartz CPO. Our results draw distinctions between CPO weakening due to: (i) second phase drag, leading to ineffective recovery in quartz; and (ii) increased transmission and localisation of strain between interconnected mica grains. In the latter case, well-connected micaceous layers take up most of the strain, weakening the rock and preventing straining of the stronger quartz matrix. Our findings suggest that rock weakening in quartz-rich crustal rocks is influenced not only by the presence of mica-rich layers but also the degree of mica grain connectivity, which allows for more effective strain localization through the entire rock mass.  相似文献   

饲料中主要能量物质对大菱鲆幼鱼生长的影响   总被引：9，自引：0，他引：9  

马爱军  陈四清  雷霁霖  陈大刚  于东祥  王立超  张少华 《海洋与湖沼》2001,32(5):527-533

于1999年6－8月，采用正交设计统计方法，对主要能量物质蛋白质、脂肪和糖类对大菱Ping幼鱼生长的影响进行研究。利用L16（4^3）正交设计了16组大菱Ping幼鱼饲料，在各级饲料中，蛋白质、脂肪和糖类的含量范围分别为36％－45％、8％－20％和0％－6％，共进行了60d的喂养实验，并对饲料及鱼体成分进行分析测定。结果表明，各主要能量物质对鱼体增重和配合饲料转化率的影响顺序为蛋白质＞糖类＞脂肪，且蛋白质的变化对增重率的影响极显著，对饲料转化率的影响显著。  相似文献   

Metamorphic P–T profile and P–T path discontinuity across the far‐eastern Nepal Himalaya: investigation of channel flow models     

T. IMAYAMA  T. TAKESHITA  K. ARITA 《Journal of Metamorphic Geology》2010,28(5):527-549

Thermobarometric data and compositional zoning of garnet show the discontinuities of both metamorphic pressure conditions at peak‐T and P–T paths across the Main Central Thrust (MCT), which juxtaposes the high‐grade Higher Himalayan Crystalline Sequences (HHCS) over the low‐grade Lesser Himalaya Sequences (LHS) in far‐eastern Nepal. Maximum recorded pressure conditions occur just above the MCT (～11 kbar), and decrease southward to ～6 kbar in the garnet zone and northward to ～7 kbar in the kyanite ± staurolite zone. The inferred nearly isothermal loading path for the LHS in the staurolite zone may have resulted from the underthrusting of the LHS beneath the HHCS. In contrast, the increasing temperature path during both loading and decompression (i.e. clockwise path) from the lowermost HHCS in the staurolite to kyanite ± staurolite transitional zone indicates that the rocks were fairly rapidly buried and exhumed. Exhumation of the lowermost HHCS from deeper crustal depths than the flanking regions, recording a high field pressure gradient (～1.2–1.6 kbar km^?1) near the MCT, is perhaps caused by ductile extrusion along the MCT, not the emplacement along a single thrust, resulting in the P–T path discontinuities. These observations are consistent with the overall scheme of the model of channel flow, in which the outward flowing ‘HHCS’ and inward flowing ‘LHS’ are juxtaposed against each other and are rapidly extruded together along the ‘MCT’. A rapid exhumation by channel flow in this area is also suggested by a nearly isothermal decompression path inferred from cordierite corona surrounding garnet in gneiss of the upper HHCS. However, peak metamorphic temperatures show a progressive increase of temperature structurally upward (～570–740 °C) near the MCT and roughly isothermal conditions (～710–810 °C) in the upper structural levels of the HHCS. The observed field temperature gradient is much lower than those predicted in channel flow models. However, the discrepancy could be resolved by taking into account heat advection by melt and/or fluid migration, as these can produce low or nearly no field temperature gradient in the exhumed midcrust, as observed in nature.  相似文献   

The cratering history of asteroid (2867) Steins     

S. Marchi  C. Barbieri  F. Marzari  H.U. Keller  P. Lamy  M. Massironi 《Planetary and Space Science》2010,58(9):1116-490

The cratering history of main belt asteroid (2867) Steins has been investigated using OSIRIS imagery acquired during the Rosetta flyby that took place on the 5th of September 2008. For this purpose, we applied current models describing the formation and evolution of main belt asteroids, that provide the rate and velocity distributions of impactors. These models coupled with appropriate crater scaling laws, allow the cratering history to be estimated. Hence, we derive Steins’ cratering retention age, namely the time lapsed since its formation or global surface reset. We also investigate the influence of various factors—like bulk structure and crater erasing—on the estimated age, which spans from a few hundred Myrs to more than 1 Gyr, depending on the adopted scaling law and asteroid physical parameters. Moreover, a marked lack of craters smaller than about 0.6 km has been found and interpreted as a result of a peculiar evolution of Steins cratering record, possibly related either to the formation of the 2.1 km wide impact crater near the south pole or to YORP reshaping.  相似文献   

吉尔吉斯斯坦水资源及其开发利用   总被引：3，自引：0，他引：3  

李湘权  邓铭江  龙爱华  章毅  雷雨 《地球科学进展》2010,25(12):1367-1075

吉尔吉斯斯坦共和国地处中亚中心,山地众多,山脉纵横,冰川广泛发育,水资源十分丰富,是中亚五国的"水塔",控制着中亚五国的水资源命脉.吉尔吉斯斯坦经济社会发展潜力巨大且发展意愿十分强烈,研究其水资源及开发利用对找寻妥善的中亚水资源问题解决之道具有十分积极的意义.分析介绍了吉尔吉斯斯坦自然地理以及与水资源形成有关的气候、地形地貌和冰川融雪概况,评价了吉尔吉斯斯坦水资源总量.然后在阐述吉尔吉斯斯坦独立以来至今的社会经济发展概况的基础上,分析介绍了其主要水资源开发工程与水力发电、用水量变化,并对吉尔吉斯斯坦水资源开发利用中存在的主要问题进行了深入剖析.  相似文献   

帕米尔东北侧中强地震前应力场动态变化特征分析   总被引：11，自引：0，他引：11       下载免费PDF全文

高国英  王海涛  温和平  魏斌 《地震工程学报》2001,23(4):389-394

依据乌恰、喀什和巴楚3个台小震综合机制解资料,分析研究了帕米尔东北侧中强地震前震源区及其附近地区应力场的动态变化过程.结果表明3个台小震综合机制解的P轴方位各自存在较明显的优势分布,这种分布与区域应力场的分布特征基本吻合.该区发生的4次6级以上地震前3个台小震综合机制解的P轴方位显示出较好的一致性,特别在伽师地震前P轴方位集中分布于N60°～74°E,与伽师强震群震源机制解的P轴方位基本相同.  相似文献   

P波初动方向变化的震时监测预报意义     

唐燕娟 《地震研究》1994,17(4):396-401

本文根据Ｐ波初动方向来判断在同一次地震群中，最大的一次地震发生后，有一次或几次地震的Ｐ波初动方向会改变，由此可以判断主震已过。此方法简单明了，在有感地震发生后能随时判断以后的Ｐ波初动方向，一旦方向改变说明不会再有大地震来了。在临震监测预报中具有一定意义。  相似文献