共查询到20条相似文献，搜索用时 93 毫秒
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һ��GPS��λ�����ֶ�ƽ����ϵ��Զ������� 总被引：4，自引：3，他引：1
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����Delaunay�������Ĵ��ģCORS��վ���������о� 总被引：1，自引：0，他引：1
???????вο???(CORS)????????????GPS???????????λ(RTK)??????????GPS??????λ?????????????? ??λ???????????????????????????????????????????е?Delaunay?????????????????????CORS????????????????????????????????????????????????ο??????????????????????????????????????????Ч??????????? 相似文献
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?????????????????????????????????????????????????????????????????????????????????????????????????????????????????沿???????????????????????????????????????????λ?????????ICP??????????????????????????????????????????????????????????????????????????????????????????????μ??????????????????????????????????????????????????Ч??? 相似文献
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??????????????????????????????????????????????????L???????????????????????????????????????????е????????????????????t???Cholesky?????е?λ?????????????????????????????????????????????????е?λ???????L???????????????е????????á????????????????????????Ч????????????????? 相似文献
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????????????λ?????????????????????λ???????γ?????г????????????????????????????????Щ???????Ч????????????????????????????????????????????????????豣???????????????????????????????????????????滮??????????????????????????????????????????????????????????????????滮???????????????????????????????????????GPS??????????????????滮?????????????????????????? 相似文献
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???????????????????к?????????????????к??????????????????????С????????????????????????????????????С?????????????????????????С?????????????????????????С?????????????????????????????????????????????????????????????????С?????????з???????????????????????????????????????????С?????????????????????????????к?????????????????????????????????????????????????λ????????????????????????λ?????????????????????????????????????з?????????????????????????????????????????,??????????С??????????????????λ??????????????????????????? 相似文献
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�ϲ�λ������ĵر������仯�����о� 总被引：10，自引：8，他引：2
??????????????????????????????????ζ??λ??????????????仯????????о????????????????????????????????仯???????????????1)??1??????????????????仯?У??????仯?????????????仯????λ??仯?????????С???????????????????С?????????????????仯?????????2?????????????????Σ??????????????????????仯???????????λ??????????????????????????????仯????????????????????????????????????仯??????????? 相似文献
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矽卡岩型多金属矿受接触带、断裂及层间破碎带等构造控制,产于接触带的矽卡岩中,其目标体和围岩在磁性、电性等物理特征方面具有一定的差异,利用合适的物探方法追索矿体走向,推断矿体的空间赋存状态,为深部揭露提供依据。高精度磁测和激电中梯测量能够快速圈定目标体引起的磁电异常在地表的投影位置;四极测深法可了解极化体的空间赋存状态;利用不同极距的联合剖面法可确定极化体的倾向等。利用综合物探方法在青海省哈得尔甘南地区和阿日特克山地区寻找矽卡岩型多金属矿效果良好,在追索矽卡岩矿化带、确定目标体产状等方面发挥着重要作用。 相似文献
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碳是自然界中常见的一种元素,其以单矿物(如石墨、金刚石)、化合物形式(如碳酸盐、二氧化碳)及生物体中的有机碳等多种形式存在。随着越来越多的深入研究,碳质物或石墨化的作用和地位也引起了广泛的关注。石墨碳质物出现在不同地壳深度的断裂带或俯冲带岩石中,特别是在一些大地震断裂带中富集。在地质变质作用过程中,随着温度的增加,非晶形碳质物转变为晶形有序化的石墨,且其石墨化过程不可逆,因此其拉曼光谱峰可定量记录峰期变质作用温度;同时,在变形过程中,石墨的特殊结构性能和力学属性能有效降低岩石强度,促进塑性变形,在快速滑动面或地震滑动面中,起到固体润滑剂作用,因此,地壳中的石墨物质对于岩石强度弱化和地震断裂滑动及演化过程具有重要意义。石墨碳质物具有低溶解性和低移动性,常作为碳汇稳定存在于深部地壳中,在地质时间尺度上,一旦碳及石墨化共同参与到岩石中,一些主要的地质过程(如俯冲作用、断裂作用、风化侵蚀、生物作用)致使石墨碳质物通过形成和破坏过程富集或释放碳到地球表面(大气圈),将显著地影响碳循环。 相似文献
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《中国海洋大学学报(英文版)》2015,(1)
In order to study buckling propagation mechanism in deep sea pipelines, the contact between pipeline's inner walls in buckling process was studied. A two-dimensional ring model was used to represent the pipeline and a nonlinear spring model was adopted to simulate the contact between inner walls. Based on the elastoplastic constitutive relationship and the principle of virtual work theory, the coupling effect of pipeline's nonlinear large deformation and wall contact was included in the theoretical analysis with the aid of MATLAB, and the application scope of the theoretical model was also discussed. The calculated results show that during the loading process, the change in external pressure is closely related to the distribution of section stress, and once the walls are contacting each other, the external pressure increases and then remains stable after it reaches a specific value. Without fracture, the pipeline section will stop showing deformation. The results of theoretical calculations agree well with those of numerical simulations. Finally, in order to ensure reliability and accuracy of the theoretical results, the collapse pressure and propagation pressure were both verified by numerical simulations and experiments. Therefore, the theoretical model can be used to analyze pipeline's buckling deformation and contact between pipeline's inner walls, which forms the basis for further research on three-dimensional buckling propagation. 相似文献
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According to well logs, core, seismic and other geological data, the authors studied the tectonic evolution stages, trap formation stages, fault and fracture development in the Bashituo area, and furthermore, analyzed the time of hydrocarbon accumulation, hydrocarbon migration pathways and related controversial issues in the study area. It is believed that the tectonic evolution in the study area can be divided into three stages, namely Late Hercynian, the Early Himalayan and the Late Himalayan. In the Late Hercynian, tectonic movement led to folding and faulting, resulting in the embryonic form of anticlinal traps. In the Early Himalayan, affected by both tectonic movement and transformation, deep faults reactivated and cut through the Lower Tertiary strata. After the Early Himalayan tectonic movement, faulting stopped and no vertical migration pathway was available. Then hydrocarbon migrated laterally along the sand bodies in the Bachu Formation and accumulated in the Carboniferous reservoirs. However, the Carboniferous accumulation was formed late, and the tectonic movement was weak at the Late Himalayan, and faults were underdeveloped, so the reservoirs in the deep Bachu Formation were not disturbed. 相似文献
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基于多尺度球面小波分析云南地区应变特征 总被引：1，自引：0，他引：1
使用GAMIT/GLOBK软件处理2011~2016年云南地区GPS区域站观测数据，扣除同震影响、区域欧拉均匀旋转矢量后，得到该区域的GPS水平速度场，并采用多尺度球面小波模型获取分解尺度分别为6、7、8和9时的云南地区GPS应变场，然后结合云南地区历史MS5.0以上地震信息，以及小江、红河等区域断裂活动情况分析该区域应变场的空间分布特征。结果显示，在区域应变场整体解算中，利用球面小波方法能够适应测站点的疏密变化，多尺度估计地表应变场。主应变、面膨胀和剪应变等分析结果与区域历史地震信息及对应区域断裂活动性质具有较好的吻合性。从应变结果看，红河断裂可能是具有重要构造意义的活动断裂，应变特征显示云南区域被红河断裂划分为2个特征区域；云南地区的鲁甸、腾冲、普洱、大理区域可能是地震活动较为剧烈的区域；小江断裂带中的嵩明区域在不同应变特征中均表现出高度异常，后期应予重点关注。 相似文献
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山东省招远市西北部原疃地区地理位置特殊,位于区域上两大断裂金矿带之间的玲珑复式岩体的核部,与西北部的郭家岭花岗闪长岩疑似为断层接触关系,金矿成矿条件优越。运用激电中梯、高精度磁法测量,基本查明了区内与金成矿有关的岩体、断裂构造的分布情况,圈定激电异常7处,其中1处异常经验证为矿致异常。应用CSAMT,SIP方法对矿带的深部进行探测,确定其沿走向及倾向均有一定延伸,对其深部异常进行钻探验证,证明深部异常仍为矿致异常。综合找矿方法在此次找矿过程中发现了矿致异常,缩小了找矿靶区,为钻探工程的部署提供了依据。 相似文献
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分析了渭河盆地新生代构造及演化特征。结合秦岭北缘断裂的断层分段性研究发现,口镇-关山断裂与秦岭北缘断裂强烈活动的断层段具有很好的空间对应关系。利用有限元模拟研究作为渭河盆地主控断裂的秦岭北缘断裂和华山山前断裂在伸展作用下对口镇-关山断裂和渭河盆地北缘断裂带其他断层的影响。结果显示,口镇-关山断裂的断层活动是秦岭北缘断裂东段作为秦岭北缘断裂中活动性较强的断层段伸展作用的构造响应,同时口镇-关山断裂作为先存构造加剧了上述影响,使其成为渭河北缘断裂带中活动强烈的断层。 相似文献