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961.
通过对玉林新一代天气雷达情况的分析,根据综合防雷设计的要求提出了玉林新一代天气雷达的具体防雷设计方法,重点突出直击雷防护及电子设备线路的防护措施,从而提高雷达站防御雷击侵害的能力,确保雷达站安全、可靠运行。 相似文献
962.
Detrital Zircon Dating of Meso- and Neoproterozoic Rocks in North China and Its Implications 总被引:4,自引:0,他引:4
Gao Linzhi Liu Pengju Yin Chongyu Zhang Chuanheng Ding Xiaozhong LIU Yanxue Song Biao 《《地质学报》英文版》2011,85(2):271-282
New dates from Meso- and Neoproterozoic strata contribute to the recently defined Precambrian stratigraphical timescale of China agreed by the Subcommission on the Precambrian System, and the National Commission on Stratigraphy of China on Nov. 24, 2009. First, the age range of the Changcheng System, including the Changzhougou, Chuanlinggou, Tuanshanzi and Dahongyu formations has been constrained to 1.8–1.6 Ga. Second, the Jixian System including the Gaoyuzhuang, Yangzhuang, Wumishan, Hongshuizhuang and Tieling formations has been constrained to 1.6–1.4 Ga. Third, an as-yet unnamed (undefined) system (1.4–1.0 Ga) is only developed in the Xiamaling Formation at the Jixian section, Tianjing. Fourth, the Qingbaikou System, including the Luotuoling and Jing’eryu formations has been constrained to 1.0–0.78 Ga. Fifth, the Nanhuan System ranges between 780–635 Ma, and the Sinian System is within 635–542 Ma. However, according to a series of SHRIMP U-Pb dates from the late Precambrian in the Jiangnan Orogen Belt in South China Platform, the constrained strata will be redefined as in the upper part of the Qingbaikou System. To aid global geodynamics, it is useful to denote a late Precambrian section with unified, precise and high-precision chronological dating; this is here defined in North China Block and Jiaoliao-Korean Block. However, the Neoproterozoic Qingbaikou study in North China will be influence in whole Meso- and Neoproterozoic in the Jiangnan Orogenic Belt in between the Yangtze Block and the Cathaysia Block in South China. 相似文献
963.
964.
The silicon isotopic composition of dissolved silicon and suspended particulate matter (SPM) were systematically investigated in water samples from the mainstem of the Yellow River and 4 major tributaries. The SPM content of the Yellow River varied from 1.4 to 38,560 mg/L, averaging 3568 mg/L, and the δ30Si of suspended particulate matter (δ30SiSPM) varied from 0.3‰ to −0.4‰, averaging −0.02‰. The major factors affecting the SPM content and the δ30SiSPM values in the Yellow River were inferred to be the mineralogical, chemical and isotopic characteristics of the sediments from the Loess Plateau and a combination of the climate and the flow discharge of the river.The major ions in the Yellow River water were Na+, Ca2+, Mg2+, HCO3−, SO42− and Cl−. High salt concentration was observed in samples from the middle and lower reaches, likely reflecting the effects of evaporation and irrigation because the Na+, Mg2+, SO42− and K+ concentrations were correlated with the Cl− concentration. The dissolved Si concentration (DSi) increased downstream, varying from 0.016 to 0.323 mM. The δ30Si of dissolved Si (δ30SiDiss) varied from 0.4‰ to 2.5‰, averaging 1.28‰. The major processes controlling the DSi and δ30SiDiss of the Yellow River are (a) the weathering of silicate rocks, (b) the formation of phytoliths in plants, (c) the evaporation of water from and the addition of meteoric water to the river system, which only affects concentrations, (d) the adsorption and desorption of aqueous monosilicic acid on iron oxide, and (e) the dissolution of phytoliths in soils.The DSi and δ30SiDiss values of global rivers vary spatially and temporally in response to changes in climate, chemical weathering intensity and biological activity. The moderately positive δ30SiDiss values observed in the Yellow River may be attributed to the higher rates of chemical weathering and biological activities that have been observed in this catchment in comparison with those of other previously studied catchments, excluding the Yangtze River. Human activities may also potentially influence chemical weathering and biological activities and affect the DSi and δ30SiDiss values of the major rivers of the world. Further river studies should be performed to gain a better understanding of the global Si isotope budget. 相似文献
965.
本文对班公湖地区中生代沙木罗组(J3—K1s)和日松组(J3r)地层的碎屑锆石进行了形态学及U-Pb年代学的研究。结果表明:锆石颗粒粒径约为100~150 μm,内部结构清晰,晶体为长柱状,自形程度较高,多数锆石不含暗色包体及浑圆形内核; 有些锆石颗粒有扇型分带结构。Th/U比值较大,多数大于0.1,均值约为0.86,说明岩浆的成因以锆石为主体,部分颗粒或晶体可能为变质成因; 锆石年龄主要分布在6个区间范围内: 1)180~100 Ma, 2)350~180 Ma, 3)600~450 Ma, 4)1100~600 Ma, 5)1800~1400 Ma, 6)2200~1800 Ma。锆石U-Pb年龄谱对应了羌塘地块经历的几次构造热事件,验证了晚侏罗世—早白垩世班公湖地区的物源主要来自其北部的羌塘地块。 相似文献
966.
967.
长江口水下三角洲137Cs最大蓄积峰的分布特征 总被引:2,自引:2,他引:0
在长江口水下三角洲地区,用137Cs进行沉积速率的测定时,一般认为137Cs最大值所在层位为1963年沉积层.本文通过建立模型.对此进行了计算验证.模型中利用日本东京地区的137Cs年平均大气沉降通量,再通过东京与上海两地的降水最进行校正,并根据不同的沉积速率和取样间隔分别计算出137Cs剖面中的最大值范围,再将理论计... 相似文献
968.
969.
基于耦合关系的干旱绿洲区农村居民点整理分区研究——以张掖市甘州区为例 总被引:1,自引:0,他引:1
以张掖市甘州区为例,利用系统科学理论与方法,研究农村居民点整理与农村社会经济之间的动态耦合规律,并以甘州区18个乡镇为研究单元,构建了农村居民点用地整理分区评价指标体系,利用熵值法确定权重,计算农村居民点整理的综合评价值,运用层次筛选法将研究区划分为5个整理区。研究结果:①甘州区农村居民点与农村社会经济的耦合度演化分为3个阶段:1995—1997年,二者不甚协调;1998—2003年,二者都处于持续、稳定、最佳协调发展状态;2004—2007年,二者处于相对稳定协调状态;目前二者处于不甚协调发展阶段。②农村居民点整理分区包括优先整理区、强化整理区、适度整理区、一般整理区和完善整理区。 相似文献
970.