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561.
黔西北某井田KARST地貌煤层底板温度受岩溶、沉积环境、构造、水文地质条件等因素的影响,存在无规律变化现象。因此在计算未测地温值时,首先将9煤层底板深度、温度、标高进行多元线性回归分析,利用多元同归关系式计算钻孔地温值,与实测值一起进行线性插值,绘制9煤层底板地温等值线图,并圈出正常温度及一、二级高温范围。 相似文献
562.
Trilobite Biostratigraphy of the lower Paleozoic (Cambrian–Ordovician) Joseon Supergroup, Taebaeksan Basin, Korea 总被引:1,自引:0,他引:1
CHOI Duck K. LEE Jeong Gu LEE Seung-Bae PARK Tae-Yoon S. HONG Paul S. 《《地质学报》英文版》2016,90(6):1976-1999
In Korea,trilobites are among the most intensively studied fossil groups in the past century and provide invaluable information about lower Paleozoic stratigraphy,paleogeography,and tectonics of the Korean Peninsula. Trilobites occur in the lower Paleozoic Joseon Supergroup of the Taebaeksan Basin which was part of the Sino-Korean Craton in the Paleozoic. The Joseon Supergroup is divided into the Taebaek,Yeongwol,and Mungyeong groups. The Taebaek and Yeongwol groups are richly fossiliferous,while the Mungyeong Group is poorly fossiliferous. Contrasting trilobite faunal contents of the Taebaek and Yeongwol groups resulted in two separate biostratigraphic schemes for the Cambrian–Ordovician of the Taebaeksan Basin. A total of 22 biozones or fossiliferous horizons were recognized in the Taebaek Group; 19 zones were established in the Yeongwol Group; and four biozones were known from the Mungyeong Group. These trilobite biozones of the Taebaeksan Basin indicate the Joseon Supergroup ranges in age from the Cambrian Series 2 to Middle Ordovician and can be correlated well with the formations of North China,South China,and Australia. 相似文献
563.
内蒙古双尖子山银多金属矿床花岗斑岩年代学、地球化学特征及构造意义 总被引:2,自引:0,他引:2
本文对内蒙古双尖子山银多金属矿床花岗斑岩进行了锆石SHRIMP U-Pb定年,并对花岗斑岩的主量元素、微量元素组成进行了分析研究。结果显示,双尖子山花岗斑岩加权平均年龄为(133.4±1.2)Ma,为大兴安岭南段早白垩世岩浆活动集中期产物;花岗斑岩SiO_2含量为68.81%~70.05%,低MgO、TiO_2,K_2O/Na_2O为0.97~1.27,较为富钾;A/CNK在0.94~1.12之间,属准铝-弱过铝系列;富集Rb、Th、U、K等大离子亲石元素(LILE),亏损Sr、P、Ti等高场强元素(HFSE);稀土总量ΣREE中等,δEu为0.55~0.62,Eu中等负异常。本文认为双尖子山银多金属矿床为多期次叠加的岩浆热液型矿床,160Ma和133Ma可能分别是岩浆活动的两个高峰期。花岗斑岩形成于陆内晚造山期-造山期后的伸展环境,蒙古-鄂霍次克洋俯冲板片在深部断离,引发软流圈物质上涌,这是导致大兴安岭南段早白垩世岩石圈伸展环境的主要机制。 相似文献
564.
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566.
黄河源区径流对气候变化的响应及敏感性分析(英文) 总被引:3,自引:1,他引:3
Response of the runoff in the headwater region of the Yellow River to climate change and its sensibility are analyzed based
on the measured data at the four hydrological stations and ten weather stations during the period 1959–2008. The result indicates
that change of temperature in the region has an obvious corresponding relationship with global warming and the changes of
annual average temperature in each subregion in the region have been presenting a fluctuant and rising state in the past 50
years. However the change of precipitation is more intricate than the change of temperature in the region because of the influences
of the different geographical positions and environments in various areas, and the change of annual precipitation in the main
runoff-producing area has been presenting a fluctuant and decreasing state in the past 50 years. And there is a remarkable
nonlinear correlativity between runoff and precipitation and temperature in the region. The runoff in the region has been
decreasing continuously since 1990 because the precipitation in the main runoff-producing area obviously decreases and the
annual average temperature continuously rises. As a whole, the runoff in each subregion of the headwater region of the Yellow
River is quite sensitive to precipitation change, while the runoff in the subregion above Jimai is more sensitive to temperature
change than that in the others in the region, correspondingly. 相似文献
567.
本文采用1984—1992年期间日本气象厅(JAM)推算出的大气激发函数序列(χ1,χ2),和美国喷气推进实验室(JPL)提供的Space93极坐标序列经过反卷积而推出的测地激发函数(ψ1,ψ2)进行了比较。同时也比较了极移(x,y)和从大气激发序列归算出(经过卷积)激发极移(m1,m2)。 相似文献
568.
采用球面几何的方法推导轴系位置误差对地平式望远镜指向、跟踪精度影响的计算模型.介绍2米级地平式望远镜轴系误差检测及数据处理方法.通过对目标星体指向、跟踪仿真,得到轴系位置误差对指向、跟踪精度影响规律,为轴系精度及轴系位置要求提供理论依据,并为后续控制修正提供参考模型. 相似文献
569.
This article discussed about snow temperature variations and their impact on snow cover parameters. Automatic temperature
recorders were used to sample at 10-minute intervals at the Tianshan Station for Snow-cover and Avalanche Research, Chinese
Academy of Sciences. 10-layer snow temperature and the snow cover parameters were measured by the snow property analyzer (Snow
Fork) in its Stable period, Interim period and Snow melting period. Results indicate that the amplitude of the diurnal fluctuation in the temperature during Snow melting period is 1.62 times greater than that during Stable period. Time up to the peak temperature at the snow surface lags behind the peak solar radiation by more than 2.5 hours, and lags
behind the peak atmospheric temperature by more than 0.2 hours during all three periods. The optimal fitted function of snow
temperature profile becomes more complicated from Stable period to Snow melting period. 22 h temperature profiles in Stable period are the optimal fitted by cubic polynomial equation. In Interim period and Snow melting period, temperature profiles are optimal fitted by exponential equation between sunset and sunrise, and by Fourier function when
solar radiation is strong. The vertical gradient in the snow temperature reaches its maximum value at the snow surface for
three periods. The peak of this maximum value occurs during Stable period, and is 4.46 times greater than during Interim period. The absolute value of temperature gradient is lower than 0.1°C cm−1 for 30 cm beneath snow surface. Snow temperature and temperature gradient in Stable period∼Interim period indirectly cause increase (decrease) of snow density mainly by increasing (decreasing) permittivity. While it dramatically
increases its water content to change its permittivity and snow density in Snow melting period. 相似文献
570.