Paleomagnetic Results of Later Paleozolic Rocks From Alashan Area of Western North China Block

In order to contribute to the Apparent Polar Wander Path (APWP) of the North China Block (NCB) , we collected paleomagnetic samples of Late Paleozoic rocks from the northern and southern margins of the Alashan (Alxa) terrane (the western part of Inner Mongolia and northern parts of Gansu and Ningxia Provinces) and adjacent regions. Laboratory work revealed different types of demagnetization behavior and isolated a higher temperature characteristic component in most of the samples. Results of IRM experiments show high thermal stability and high coercivities for the magnetic carriers in these rocks. The characteristic component passed the fold and/or reversal tests, suggesting that the characteristic components were probably primary. On the basis of comparing the paleomagnetic results with the geologic evidence, we discuss the tectonic implications. In the Late Paleozoic, the Alashan region had been part of the NCB and was not connected with the northern and southern blocks. During the Carboniferous Alash     

阿拉善及邻区石炭二叠系古地磁学研究及意义

本文对分布于华北块体西部的阿拉善及河西走廊地区的石炭系和二叠系进行了详细的古地磁学研究。对岩石标本剩磁载体和剩磁稳定性研究以及对所分离出的高温特征分量的统计检验结果表明,特征分量代表了原生剩磁分量,从而得到这一地区在晚古生代的地磁极位置,补充了中国华北块体的APWP,揭示了华北块体西部大陆内部变形的特点。结果表明,在晚古生代华北块体徘徊于赤道附近,并非冈瓦纳古陆的一部分;同时证明阿拉善及邻区相对于鄂尔多斯地区的旋转导致贺兰山槽区的剪刀型闭合。     

K促进的Fe/椰壳炭催化剂对甲烷氮气常压合成氨性能的影响

采用等体积浸渍法制备了一系列催化剂用于甲烷氮气常压合成氨反应.对Si O2、γ-Al2O3、煤质柱状炭、椰壳活性炭为载体的Fe基催化剂的活性评价结果显示椰壳炭载体最优;通过对Zr、Ce、K等多种助剂的筛选,发现K促进的Fe基催化剂氨生成速率最高.利用XRD、SEM、BET等手段对载体和催化剂进行表征,结果表明椰壳炭具有规则孔道且孔容增大,催化剂还原后有新晶相KFe O2生成.最后在固定床微分反应器中,考察了常压合成氨催化剂的负载顺序及最优工况.结果表明,在常压700℃、VCH4/VN2=2/1、空速为2 800 m L/h时,催化剂3%K-5%Fe/椰壳炭的氨生成速率最高可达1.04×10-6mol·g-1·s-1,是现有文献值的83.5倍,将具有深远的工业应用前景.     

油井样品NMR T2谱的影响因素及T2截止值的确定方法

T₂ 谱是核磁共振（NMR）测、录井技术应用与解释、评价的基础. 岩样T₂ 谱受仪器测量参数、样品性质（岩性、颗粒大小、样品粒度、样品干湿状态、孔隙流体含量及性质、磁化率、润湿性）及地层水矿化度等因素的影响. T₂ 截止值是T₂ 谱中最重要的参数之一,选取的科学性与准确性直接影响到核磁共振测量结果. 通过文献查询,对T2 谱的影响因素及T₂ 截止值的确定方法进行了分析.