Very Low-Grade Metamorphism of Clastic Rocks from the Meso-Neoproterozoic and the Paleozoic along the Profile Yueyang-Linxiang in Northeastern Hunan Province and Its Geological Implications   总被引：1，自引：0，他引：1  

WANG Hejing  YUAN Lei  WANG Ling  ZHOU Zhao  AN Jiali 《《地质学报》英文版》2016,90(5):1743-1753

This study uses illite crystallinity,chlorite crystallinity,illite polytypes,the b_0 cell-dimension of K-white mica,clay mineral assemblages and mineral geothermo-geobarometers to investigate the overprint of diagenesis and metamorphism on the Meso-Neoproterozoic and the Lower Paleozoic along the profile Yueyang-Linxiang in northeastern Hunan Province,China.Illite crystallinity Kbler index(KI) of the 2μm fractions ranges from 0.225 to 0.485°Δ2θ while chlorite crystallinity Arkai index(AI) ranges from 0.244 to 1.500°Δ2θ.This indicates that the Meso-Neoproterozoic and the Lower Paleozoic along the profile Yueyang-Linxiang were overprinted with diagenesis and anchi- to epimetamorphism.Peak metamorphic temperature is estimated with the IV site chlorite geothermometer roughly at 360℃.The b_0 cell dimension values of illites(K-mica) range from 0.9002 to 0.9054 nm and,on average,at 0.9030 nm for the Meso-Neoproterozoic.Based on cumulative frequency curves of illite(K-mica) b_0 cell dimension,the peak metamorphic pressure of the MesoNeoproterozoic along the profile Yueyang-Linxiang is derived of an intermediate pressure type.Most illites occur in the 2M_1 polytype and some of them in a mixture of 2M1+1M types especially those in the Paleozoic.This result partly agrees with the conclusion of the lower greenschist and greenschist facies of the Lengjiaxi and Banxi Groups.However,it is not agreed with the sedimentary cover from the Sinian to the Lower Paleozoic or from the Banxi Group to the Lower Paleozoic.Crustal thickening due to "collision" between the Yangtze and Cathaysia blocks led to an increase in the thickness of the Meso-Neoproterozoic to ca.14 km and resulted in a temperature increase in those rocks due to burial.The very low grade to low grade metamorphism overprinting the Meso-Neoproterozoic implies that the so called "Chiangnania or Jiangnan orogen" was no relative with the "Grenvillian orogeney;instead,it might be a continuous amalgamation product between the Yangtze and Cathaysia blocks.  相似文献   

同址观测重力仪与地震仪地震频段噪声水平比较     

李航  陈晓东  徐建桥  孙和平  张苗苗  韩宇飞 《大地测量与地球动力学》2020,40(8):843-848

选用拉萨台超导重力仪、昆明和恩施台gPhone重力仪以及各台站同址观测的STS-1和STS-2.5地震仪观测数据,计算所有仪器在地震频段（0.1～100 mHz）的噪声水平,并分别进行比较。结果表明,1 mHz以上时,拉萨台超导重力仪噪声水平略高于同址观测的地震仪结果,而1 mHz以下则相反;0.5 mHz以上时,恩施和昆明台gPhone重力仪的噪声水平高于地震仪结果,0.1～0.5 mHz时则与地震仪结果接近。用带通滤波处理和未滤波处理2种方法计算地震噪声等级（seismic noise magnitude, SNM）,结果表明,采用带通滤波方法计算得到的SNM值更小,且随月份的变化更加平缓。  相似文献   

The activity of Vesuvius in the next millennium     

Antonino Palumbo 《Journal of Volcanology and Geothermal Research》1999,88(1-2)

The time distribution of the historical eruptions of Vesuvius allows the forecasting of the activity of the volcano for the next millennium according to three independent models. The next event with volcanic explosivity index (VEI)=4 is likely to occur during the next few decades followed by a decreasing number of smaller eruptions in the successive few centuries and by a very long period of quiescence up to the beginning of the following fourth millennium when the next Plinian event (VEI=5) might occur.  相似文献   

VLBI观测资料解算地球自转参数精度分析     

钱炜  岳建平  单丽杰  韩宸宇 《大地测量与地球动力学》2021,41(12):1245-1248

为分析VLBI观测资料解算地球自转参数的精度,根据VLBI观测原理及其误差方程,分别利用2020年VLBI观测数据及CONT17连续加密观测的XA、XB两种频率通道数据解算地球自转参数,并以EOP14 C04序列作为计算外符合精度的参考序列。结果表明,VLBI观测数据解算地球自转参数各分量的外符合精度均能满足高精度要求,比较解算结果与同时段GPS连续数据的解算结果发现,两者精度总体处于同一水平;CONT17观测的XA、XB两种频率通道数据解算极移时精度相当,但前者在稳定性及解算UT1-UTC序列精度上具有较大优势。  相似文献   

甚低频/低频人工源电波信号地震应用研究进展          下载免费PDF全文

张学民 《地震学报》2021,43(5):656-673

甚低频/低频人工源电波作为一种主动源发射的通讯导航信号,因其长距离波导传播的特性在地-电离层观测及应用中表现出极大的优势.本文总结了二十世纪末以来基于甚低频/低频(VLF/LF)电波观测技术及其数据分析方法、典型震例及统计研究成果、圈层耦合机理等方面的研究进展,并通过探讨其应用成果的快速积累及前兆扰动起源等研究难点,展...  相似文献   

SEDIS IV型短周期自浮式海底地震仪数据校正方法   总被引：6，自引：0，他引：6  

薛彬  阮爱国  李湘云  吴振利 《海洋学研究》2008,26(2):98-102

利用15台SEDISIV型短周期自浮式海底地震仪在南海中、北部地壳深部结构调查中所获得的资料,探讨了海底地震仪数据校正的方法和校正后的效果,结果表明:使用该地震仪所获得的原始资料经过放炮时间、炮点坐标数据局部化、海底地震仪位置误差以及记录时间漂移4方面的校正后,数据更趋合理,误差显著降低。放炮时间的校正消除了时钟漂移和时间延迟的误差;炮点坐标数据局部化处理消除了炮点位置整体趋势性偏移的现象;试错法进行位置误差和记录时间的精细校正时,时间漂移的校正量值约为几个到十几个毫秒,位置校正的量值仅在几米到数百米之间,实测数据所绘曲线的形态和位置都与理论曲线十分吻合,可见校正后误差显著降低。  相似文献   

用直接法分析超大型浮体的水弹性响应   总被引：4，自引：2，他引：2  

张淑华  韩满生 《海洋工程》2004,22(1):9-18

探讨了浮舟桥型超大型浮体结构的水弹性响应分析问题。将超大型浮体结构简化成弹性平板模型,用压力分布法计算流体压力,用直接法计算流体-结构系统,给出了它们的数学计算模型。计算表明本计算方法和程序是正确的,并能保证充分的精度,进而计算了更大尺度的超大型浮体,分析了波长、波向等对响应振幅的影响。  相似文献