羌塘盆地基底地层及大地构造性质     

祁江豪  郭兴伟  温珍河  郑求根  冯岩  伊飞 《海洋地质前沿》2011,(9):52-59

根据不同学者在盆地基底地层中所得出的锆石同位素测年数据进行统计分析,结合前人对羌塘地区大地构造方面的研究成果得出:羌塘盆地中央隆起带出露的变质岩基底可能经历过泛非时期构造热事件的作用,羌塘块体在演化过程中受到了南部冈瓦纳大陆的影响,这对于了解本地区的大地构造背景以及对古特提斯缝合带的研究有所帮助.  相似文献   

共反射面元叠加技术在南海北部莺—琼盆地中的应用     

袁全社  李列  柴继堂  邓勇  李振春 《海洋地质前沿》2011,(10)

随着莺—琼盆地油气勘探开发的不断深入,2 700m以下的中深层地震资料品质迫切需要提高,而改善信噪比提高成像质量则是需要深入研究的重点内容之一。基于共反射面元(CRS)叠加在改善中深层地震资料信噪比方面具有理论和技术应用优势,由于考虑了反射层的局部特征和第一菲涅耳带内的全部反射,对复杂地质问题的适应性得以增强,真正实现了高信噪比叠加,从而改善中深层低信噪比区的成像质量。通过理论研究分析、模型试处理及莺—琼盆地实际地震资料处理中具体的应用与试验,取得了明显的效果,即该区中深层地震资料信噪比显著增强,大大提高了解释的可靠程度。总之,共反射面元叠加技术在莺—琼盆地具有较高的推广应用价值。  相似文献   

Photosynthetic efficiency, cell volume, and elemental stoichiometric ratios in Thalassirosira weissflogii under phosphorus limitation     

��ʤ  ��־��  ����  ����  ��ɭ�� 《中国海洋湖沼学报》2011,29(5):1048-1056

Nutrient limitation is known to inhibit growth and metabolism and to alter elemental stoichiometric ratios in phytoplankton. In this study, physiological changes in Thalassirosira weissflogii were measured under different dissolved inorganic phosphate (DIP) regimes in semi-continuous cultures to revisit the utility of the Redfield ratio for assessing nutrient limitation. The results showed that cell size increased with decreasing DIP availability. In the P-depleted treatment (f/2-P) the cell size was 1.48 times larger than that in the P-limited (f/100) treatment and 2.67 times larger than that in the P-saturated treatment (f/2 and f/10). The fucoxanthin to chlorophyll a ratio (Fuco/chl a) was relatively stable (about 0.3) in P-saturated cultures and was 10 times higher than that in P-limited and P-depleted cultures. During the experimental period, the photosynthetic efficiency index, ?F/Fm′, was relatively stable at ~0.50 in the P-saturated cultures, but quickly declined with decreasing DIP availability. Although cellular P content showed a significant difference between the P-saturated culture (1.6 pg/cell) and the P-limited culture (0.7 pg/cell), the N/P ratio in T. weissflogii did not show a trend with DIP availability and fluctuated slightly around 25. Our results suggest that cell division in T. weissflogii is not strictly size-gated but is probably regulated by a biochemical, and hence, an elemental stoichiometric ratio threshold, and that deviation of the cellular N/P ratio from the Redfield ratio is not a reliable indicator of algal nutrient stress.  相似文献   

Effect of nitrogen to phosphorus ratios on cell proliferation in marine micro algae     

张青田  胡桂坤 《中国海洋湖沼学报》2011,(4)

The ratio of nitrogen/phosphorus (N/P) is known to affect cell proliferation of some marine micro algae. We evaluated the effect of N/P ratios on the proliferation and succession of phytoplankton using five marine micro algae species. We used two sources of nitrogen, NH4Cl (N1) and urea (N2), and a single source of phosphorous, NaH2PO4(P). The optimal N/P ratio that differed among the five species was affected by the source of nitrogen, being as follows (N1/P, N2/P in order): Thalassiosira sp. (30/1, 20/1),...  相似文献   

基于投入产出模型的旅游消费对经济增长的动态影响研究     

周文丽 《地域研究与开发》2011,30(3):79-83,88

基于投入产出模型,利用中国《2002年部门投入产出表》,定量测度了1997—2007年间我国城乡居民国内旅游消费对国民经济及各部门产出增长的贡献率及其变化,并提出相应的建议。研究结论:(1)城镇居民国内旅游消费对经济增长的贡献在上升,农村居民的贡献在下降,总体国内旅游消费对经济增长的贡献在下降。(2)城乡居民国内旅游消费对各产业产出增长贡献从大到小依次为:旅游业、住宿和餐饮业、交通仓储和邮政业、金融保险业、其他服务业、房地产业和批发零售业。(3)我国旅游业发展八分靠国内旅游,二分靠国际旅游;国内旅游消费结构中,非基本消费比重较小,亟待提高。  相似文献   

Domainal fabrics of hematite in schistose,shear zone-hosted high-grade Fe ores: The product of the interplay between deformation and mineralization     

《Journal of Structural Geology》2013

Schistose high-grade hematite orebodies (>64 wt % Fe) in the Iron Quadrangle, Minas Gerais, were formed in shear zones by hydrothermal alteration of the Paleoproterozoic Cauê BIF during the Transamazonian orogenesis. The ore is comprised of platy hematite (specularite) grains that define the foliation and overprint a relict banded martite-hematite fabric resembling, at first sight, a mylonite. The EBSD analyses of a m-scale schistose orebody from the Pau Branco mine show that specularite grew as elongated plates with the (00.1) plane parallel to the foliation. The population of the measured grain aspect ratio (GAR) is homogenous in different scales, and the longest axes of the crystals align with the stretching lineation (L//X) building continuous domains, or anastomose around stretched iron oxide aggregates and rootless fold hinges. The pole figure of the (00.1) plane shows usually a maximum centered on the pole of the foliation Z often elongated on a girdle perpendicular to the lineation L. The {10.4} pole figure has the configuration of a symmetric cleft girdle and the corresponding {11.0} and {10.0} pole figures present well developed girdles parallel to the foliation with an elongated maximum centered on X. Microstructures associated with crystal-plastic behavior and dynamic recrystallization are missing and the fabric of the orebody probably results from precipitation of strain-controlled oriented hematite plates and anisotropic syntaxial growth of favorably oriented grains with the intervention of hydrothermal fluids during Fe enrichment. The shear zone provided pathways for the percolation of mineralizing fluids under temperatures that varied from 140 to 350 °C or higher, under ductile or ductile–brittle conditions. The orthorhombic fabric and CPO (crystallographic preferred orientation) of the ore nevertheless contrast with the asymmetry of simple shear as observed in the torsion experiments by Siemes et al., 2010, Siemes et al., 2011, probably due to volume loss and possibly a flattening component of deformation in the ore zone.  相似文献   

X射线荧光光谱法测定高锶高钡的硅酸盐样品中主量元素   总被引：6，自引：5，他引：1  

李迎春  周伟  王健  屈文俊 《岩矿测试》2013,32(2):249-253

用百分总和检查硅酸盐岩石全分析数据的质量是分析工作者的传统做法,但对于微量元素含量较高的样品,采用X射线荧光光谱法(XRF)进行测定,如果不考虑微量元素的含量及其对主量元素基体效应的影响,往往会使主量元素含量更加偏离真实值。本文针对Sr、Ba含量较高的硅酸盐样品,通过人工配制标准样品,扩大了Sr、Ba校准曲线的定量范围,主量元素校准中加入Sr、Ba的基体校正系数,达到了主量元素定量更加准确可靠的实际效果。采用此方法分析国家标准物质,各主量元素的精密度(RSD)均小于2%;分析不参加回归的标准物质和人工配制的标准样品,主量元素的测量值与标准值(或参考值)基本一致。该方法可以满足硅酸盐的测定要求,主量元素各项结果的加和能够达到《地质矿产实验室测试质量管理规范》的一级标准(99.3%～100.7%)。  相似文献   

青海虎头崖多金属矿床地球化学特征及成矿-控矿因素研究   总被引：3，自引：1，他引：2  

张爱奎  刘光莲  丰成友  莫宣学  杨六成  刘永乐  何书跃  马永寿 《矿床地质》2013,32(1):94-108

虎头崖铜铅锌多金属矿床的成矿作用十分复杂,成矿-控矿因素仍不明,已成为制约找矿突破的瓶颈.鉴于此,笔者对该矿床的地质、地球化学特征和侵入岩年龄及地球化学开展了研究.结果表明,Ⅵ矿带二长花岗岩LA-MC-I CP-MS锆石U-Pb同位素年龄为(217.5±1.1) Ma(MSWD=1.4).Ⅵ矿带和Ⅱ矿带二长花岗岩钾、钠含量均较高,w(K2O)大于w(Na2O),分异程度较高,稀土元素球粒陨石标准化曲线向右缓倾斜,强烈富集LILE,中等富集HFSE,贫Ti、Ba,具有后碰撞阶段岩石的特点.成矿受侵入岩岩浆源区、演化方式,地层,构造,以及岩体与围岩接触方式的综合控制.源区具有地幔物质贡献的Ⅵ矿带二长花岗岩,成矿作用较强,主要形成近接触带矽卡岩型和远接触带矽卡岩型Cu-Pb-Zn多金属矿.而壳源特征为主的Ⅱ矿带二长花岗岩成矿能力较弱,主要形成矽卡岩型Sn、Mo、Fe等矿产.  相似文献   

新疆祁漫塔格柯可卡尔德钨锡矿床控矿构造及 ⁴⁰Ar-³⁹Ar年代学研究   总被引：1，自引：0，他引：1  

丰成友  李国臣  李大新  周安顺  李洪茂 《矿床地质》2013,32(1):207-216

位处新疆东昆仑祁漫塔格地区的白干湖是中国西部最新探明的一个具超大型远景规模的钨锡矿田,柯可卡尔德是其中勘查程度最高、规模最大的钨锡矿床.文章在对柯可卡尔德钨锡矿地质特征详细野外调研和剖析的基础上,重点开展了控矿构造和白云母40Ar-39Ar定年研究.结果表明,该矿区内构造活动强烈且具多期次性,可划分为成矿前向西右旋剪切构造、成矿期以NE向为主的左旋张扭性断裂和成矿后近SN向正断层性质断裂等3期.应用白云母40 Ar-39 Ar同位素测年技术,分别测得了强云英岩化钨锡矿化花岗岩脉内白云母的积分年龄为(411.7±2.6) Ma,等时线年龄为(411.8±4.7) Ma(n=8,MSWD=0.21);黑钨矿-石英脉垂直脉壁生长的片状白云母的积分年龄为(412.8±2.4) Ma,等时线年龄为(414.6±3.9) Ma(n=10,MSWD=0.22),厘定了该矿床的成矿时代为晚志留世,认为其形成于东昆仑地区加里东造山旋回的后碰撞构造阶段.  相似文献   

金红石U-Pb同位素定年技术研究   总被引：4，自引：0，他引：4  

周红英  李怀坤  崔玉荣  耿建珍  张健  李惠民 《地质学报》2013,87(9):1439-1446

本文系统阐述了金红石U-Pb同位素定年的同位素稀释热电离质谱法(ID-TIMS)和激光烧蚀多接收器电感耦合等离子体质谱法(LA-MC-ICP-MS)两种方法,讨论了这两种方法的优点和局限性.利用LA-MC-ICP-MS验证了山西代县洪塘金红石矿区金红石的U-Pb同位素年龄的均一性;利用ID-TIMS对洪塘矿区金红石进行了U-Pb同位素精确定年,获得207pb/206 Ph表面年龄加权平均值:1806±2 Ma(MSWD=2.3,n=6),不一致线的上交点年龄:1808±7 Ma(MSWD=0.20,n=6);并对金红石ID-TIMS U-Pb同位素测年和LA-MC ICP MS U-Pb同位素测年结果进行了对比研究.利用高精度的ID-TIMS U-Pb同位素测年和LA-MC-ICP-MS U-Ph同位素测年方法均有望获得准确可靠的金红石形成年龄.  相似文献