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181.
位于中缅毗邻区的金腊铅锌银多金属矿田大地构造上处于保山—掸泰地块东缘,勐统—耿马—西盟元古宙—古生代被动大陆边缘活动带南段。与矿化有关的花岗岩(简称金腊花岗岩)包括老厂似斑状角闪二长花岗岩、勐林山似斑状黑云二长花岗岩和南腊碱长花岗斑岩。文中系统研究了上述岩石的主量元素、稀土元素、微量元素、成矿元素和锆石U-Pb同位素年龄等特征,从构造岩浆演化的角度,探讨上述岩体之间内在联系、成因演化以及与成矿的关系:(1)在金腊花岗岩三种岩石类型中,老厂似斑状角闪二长花岗岩和勐林山似斑状黑云二长花岗岩的锆石同位素U-Pb年龄皆为(45±1)Ma,形成于岩浆结晶分异早期阶段的深成环境,而南腊碱长花岗斑岩的锆石同位素U-Pb年龄为(43.41±0.78)Ma,形成于岩浆结晶分异晚期阶段的浅成环境。(2)主量元素和微量元素(稀土元素和某些微量元素(Zr/Hf、Nb/Ta、Rb/Sr、Rb/Ba、K/Rb、(Rb/Yb)N、Sr*、K*和Zr*)),结合U-Pb同位素定年研究表明,本区花岗岩形成于喜马拉雅同碰撞造山成矿作用末期局部拉张构造环境,并分别代表了构造岩浆演化过程中不同演化阶段岩浆分异结晶的产物。(3)上述三类花岗岩样品皆位于S型花岗岩区,但从老厂似斑状角闪二长花岗岩,勐林山似斑状黑云二长花岗岩,到南腊碱长花岗斑岩,样品分布逐渐远离"I"型花岗岩和"S"型花岗岩的分界线,这表明自老厂似斑状角闪二长花岗岩至勐林山似斑状黑云二长花岗岩,到南腊碱长花岗斑岩幔源组分逐渐减少。(4)相对中国花岗岩,南腊碱长花岗斑岩不仅更富集W、Cu、Bi、Sb、Mo、Sn、Ag、Pb和Au等成矿元素,而且还强烈富集F、B和As等矿化剂元素,因此,碱长花岗斑岩是最有成矿远景的岩体。 相似文献
182.
Sparsity constrained deconvolution can improve the resolution of band-limited seismic data compared to conventional deconvolution. However, such deconvolution methods result in nonunique solutions and suppress weak reflections. The Cauchy function, modified Cauchy function, and Huber function are commonly used constraint criteria in sparse deconvolution. We used numerical experiments to analyze the ability of sparsity constrained deconvolution to restore reflectivity sequences and protect weak reflections under different constraint criteria. The experimental results demonstrate that the performance of sparsity constrained deconvolution depends on the agreement between the constraint criteria and the probability distribution of the reflectivity sequences; furthermore, the modified Cauchyconstrained criterion protects the weak reflections better than the other criteria. Based on the model experiments, the probability distribution of the reflectivity sequences of carbonate and clastic formations is statistically analyzed by using well-logging data and then the modified Cauchy-constrained deconvolution is applied to real seismic data much improving the resolution. 相似文献
183.
对全国自动地震速报系统进行了初步的评估. 通过2010年1月1日—2011年12月31日的自动定位结果与全国正式目录的对比, 分别得出了3套自动定位系统总体误差以及全国和全球的误差插值图, 并对结果进行了总结. 同时, 还针对3套自动定位系统的漏报和误报情况进行了分析和讨论. 总体来说, 现阶段自动地震速报系统整体上对于首都圈地区M≥3.0, 国内其它地区M≥4.0(部分台站稀疏的西部地区M≥5.0), 国外M≥7.0的地震基本可以达到全面覆盖的程度, 可以作为正式地震速报的参考, 对于建立“自动报—正式报”的两级地震速报制度能提供有力的技术支撑. 相似文献
184.
The detection and identification of the seabed cable is becoming an important task in the marine engineering. The features of the magnetic anomaly can be used to detect the existence of the seabed cable. The magnetic field model is presented, and the consistency of the magnetic anomaly distribution between the simulation of the model and the observed data is verified. The comparison shows that the seabed cable can be effectively detected and identified with reasonable method. 相似文献
185.
At present, there exist two methods used to recover the bathymetry from altimeter data, i. e. the deterministic method and the stochastic method. In this paper, the principles of the two methods are introduced first. Then according to the theory of least-square collocation, a modified statistical model for recovering bathymetry from altimeter data is proposed. The new model has been used for computing the ocean depth in the South China Sea from altimeter-derived gravity anomalies. Finally the predicted depths are compared with the ship-borne depth. It shows that they agree with each other very well. 相似文献
186.
On the basis of an analysis of the error sources in multibeam echosounding system, a data processing method for compensating systematic errors in multibeam survey is proposed. In order to improve the accuracy of overall swath, a data fusion technique using single beam survey data as control information for single beam and multibeam echosounding is then presented. Some questions involved in solving the adjustment problem, such as its feasibility and the numerical stability, are discussed in detail, and a two-step adjustment method is suggested. Finally, a practical survey data set is used as a case study to prove the efficiency and reliability of the proposed methods. 相似文献
187.
188.
通过对北大西洋IODP U1313站深海沉积序列高密度取样和粒度分析,利用粒级-标准偏差变化算法和EMD方法提取了对环境敏感粒度组分并探讨了气候变化的周期.本文粒度组分可分为细组分(<1.73μm,组分Ⅰ)和粗组分(>1.73μm,组分Ⅱ),其中粗组分又分为组分Ⅱa(1.73 ~ 34.26μm)和组分Ⅱb(>34.26μm).综合分析认为:组分Ⅰ为西风环流搬运堆积形成,组分Ⅱ为洋流搬运下沉积形成,组分Ⅱb虽然含量较低,但能指示冰漂砾事件的发生.比值曲线组分Ⅰ/组分Ⅱ和组分Ⅰ/组分Ⅱa波动幅度较大,可作为反映古气候冷暖波动的敏感指标.对组分Ⅱ、组分Ⅰ/组分Ⅱ进行EMD分解,结果表明:在本研究时段内,两指标对地球轨道三要素的周期体现均不明显,而2ka(2.12ka和2.15ka)的亚轨道千年周期是主要的周期之一.依据上述多个指标的波动情况,把研究剖面69.93 ~ 115.18mcd(1471.53~2415.60ka)分为9个古气候变化阶段:A阶段(1471.53~1640.09ka),对应深海氧同位素阶段(MIS)49~ 57,冰期和间冰期迅速转换,发生多次IRD事件;B阶段(1640.09~ 1865.57ka),对应MIS 58 ~ 69,间冰期显著而冰期不明显;C阶段(1865.57~1914.70ka),对应MIS 70~72,冰期显著而间冰期不明显;D阶段(1914.70~2021.13ka),对应MIS 73~76,冰期不显著;E阶段(2021.13~2092.21ka),对应MIS 77~78,冰期显著,发生多次IRD事件;F阶段(2092.21 ~ 2226.43ka),对应MIS 79~85,间冰期显著;G阶段(2226.43 ~2261.53ka),对应MIS 86期,发生多次IRD事件;H阶段(2261.53~ 2384.61ka),对应MIS 87~93,冰期不显著而间冰期显著;Ⅰ阶段(2384.61 ~2415.60ka),对应MIS 94 ~ 95,发生多次IRD事件. 相似文献
189.
190.
Wei Yang Bai-quan Lin Yong-an Qu Shuai Zhao Cheng Zhai Li-li Jia Wu-qiang Zhao 《International Journal of Coal Geology》2011,85(3-4):300-306
In this paper, an equation correlated with normal stress and permeability was developed and FLAC3D software was used to investigate the rock mass stress evolution and distribution to understand the methane flow characteristics. Research results show that the rock mass under the protective coal seam can be divided into three belts (zones) in the vertical direction, including total de-stressed belt, vertical de-stressed belt and original stress belt. Methane in the total de-stressed belt can flow into the working face of protective coal seam by its own pressure gradient. Methane in the vertical de-stressed belt can only be extracted by boreholes. In the horizontal direction, the rock mass was also divided into five zones, including original zone, compression zone, expansion zone, recovering zone and re-compacted zone, which have been proved correct by the field experiments. The rock mass permeability in the de-stressed belts doesn't increase until stepping into the expansion zone, and from then on higher concentration of methane can be extracted. The methane in original regions is difficult to extract because rock stresses stay the same. The division of “three belts and five zones” reveals the rock mass stress and permeability distribution and evolution and supplies theoretical guidance for relieved methane control. 相似文献