Linear and Nonlinear Time Domain Block Equalizers on MIMO Frequency Selective Channels

Single-Carrier (SC) transmission with the same bandwidth as Multi-Carrier (MC) transmission (such as OFDM) may have far shorter symbol duration and is considered to be more robust against time selective fading. In this paper, we proposed the novel equalization and signal separation schemes in time domain for short block length transmission, i.e., Block Linear Equalization (BLE) and Block Nonlinear Equalization (BNLE) on MIMO frequency selective fading channels. The proposed BLE uses the MMSE based inverse matrix in time domain and the BNLE utilizes the QRD-M (QR Decomposition with M algorithm) with appropriate receiver complexity. We compared the computational complexity among the conventional SC-FDE (Frequency Domain Equalization) scheme and the proposed equalizers. We also used the Low-Density Parity Check (LDPC) decoder concatenated to the proposed BLE and BNLE.

Geochronology and geochemistry of Cretaceous-Eocene granites,Tengchong Block(SW China):Petrogenesis and implications for Mesozoic-Cenozoic tectonic evolution of Eastern Tethys

The Early Cretaceous-Early Eocene granitoids in the Tengchong Block record the evolutionary history of the Mesozoic-Cenozoic tectono-magmatic evolution of Eastern Tethys.(a)The Early Cretaceous granitoids with relatively low(^(87)Sr/^(86)Sr)iratios of 0.7090-0.7169 andε_(Nd)(t)values of-9.8 to-7.8 display metaluminous,calc-alkaline dominated by I-type granite affinity and hybrid mantle-crust geochemical signatures.They may have been derived from melting of the subducted Meso-Tethyan BangongNujiang oceanic crust with terrigenous sediments in an arc-continent collisional setting.(b)The Late Cretaceous-Paleocene granitoids with relatively high(^(87)Sr/^(86)Sr)iratios of 0.7109-0.7627,andε_(Nd)(t)values of-12.1 to-7.9 exhibit metaluminous to peraluminous,calc-alkaline dominated by S-type granite affinity and hybrid Lower-Upper crust geochemical signatures,which may be originated from partial melting of the Meso-Proterozoic continental crust in the collision setting between the Tengchong Block and Baoshan Block.(c)The Early Eocene granitoids have metaluminous,calc-alkaline I-type and S-type granites dual affinity,with relatively high(^(87)Sr/^(86)Sr)iratios of 0.711-0.736,ε_(Nd)(t)values of-9.4 to-4.7,showing crust-mantle mixing geochemical signatures.They may have been originated from partial melting of the late Meso-Proterozoic upper crustal components mixed with some upper mantle material during the ascent process of mantle magma caused by the subduction of the Neo-Tethyan Putao-Myitkyian oceanic crust,and collision between the Western Burma Block and the Tengchong Block.It is these multi-stage subductions and collisions that caused the spatial and temporal distribution of the granitic rocks in the Tengchong Block.

Frequency Domain Adaptive Learning Algorithm for Thoracic Electrical Bioimpedance Enhancement

The Thoracic Electrical Bioimpedance(TEB)helps to determine the stroke volume during cardiac arrest.While measuring cardiac signal it is contaminated with artifacts.The commonly encountered artifacts are Baseline wander(BW)and Muscle artifact(MA),these are physiological and nonstationary.As the nature of these artifacts is random,adaptive filtering is needed than conventional fixed coefficient filtering techniques.To address this,a new block based adaptive learning scheme is proposed to remove artifacts from TEB signals in clinical scenario.The proposed block least mean square(BLMS)algorithm is mathematically normalized with reference to data and error.This normalization leads,block normalized LMS(BNLMS)and block error normalized LMS(BENLMS)algorithms.Various adaptive artifact cancellers are developed in both time and frequency domains and applied on real TEB quantities contaminated with physiological signals.The ability of these techniques is measured by calculating signal to noise ratio improvement(SNRI),Excess Mean Square Error(EMSE),and Misadjustment(Mad).Among the considered algorithms,the frequency domain version of BENLMS algorithm removes the physiological artifacts effectively then the other counter parts.Hence,this adaptive artifact canceller is suitable for real time applications like wearable,remove health care monitoring units.

A POCS-Based Algorithm for Blocking Artifacts Reduction

An algorithm for blocking artifacts reduction in DCT domain for block-based image coding was developed. The algorithm is based on the projection onto convex set （POCS） theory. Due to the fact that the DCT characteristics of shifted blocks are different caused by the blocking artifacts, a novel smoothness constraint set and the corresponding projection operator were proposed to reduce the blocking artifacts by discarding the undesired high frequency coefficients in the shifted DCT blocks. The experimental resuhs show that the propo,sed algorithm outperforms the conventional algorithms in terms of objective quality, subiective quality, and convergence property.

SINGULAR INTEGRALS ALONG SURFACES ON PRODUCT DOMAINS

In this paper, we study the mapping properties of singular integral operator along surfaces of revolution. We prove Lp bounds (1 < p < ∞) for such singular integral operators as well as for their corresponding maximal truncated singular integrals if the singular kernels are allowed to be in certain block spaces.

Detection of Underwater Objects by Adaptive Threshold FCM Based on Frequency Domain and Time Domain

According to the characteristics of sonar image data with big data feature, In order to accurately detect underwater objects of sonar image, a novel adaptive threshold FCM (Fuzzy Clustering Algorithm, FCM) based on frequency domain and time domain is proposed. Based on the relationship between sonar image data and big data, Firstly, wavelet de-noising method is used to smooth noise. After de-noising, the sonar image is blocked and each sub-block region is processed by two-dimensional discrete Fourier transform, their maximum amplitude spectrum used as frequency domain character, then time domain of mean and standard deviation, frequency domain of maximum amplitude spectrum are taken for character to complete block k-means clustering, the initial clustering center is determined, after that made use of FCM on sonar image detection, based on clustered image, adaptive threshold is constructed by the distribution of sonar image sea-bottom reverberation region, and final detection results of sonar image are completed. The comparison different experiments demonstrate that the proposed algorithm get good detection precision and adaptability.

Weber Law Based Approach for Multi-Class Image Forgery Detection

Today’s forensic science introduces a new research area for digital image analysis formultimedia security.So,Image authentication issues have been raised due to the wide use of image manipulation software to obtain an illegitimate benefit or createmisleading publicity by using tempered images.Exiting forgery detectionmethods can classify only one of the most widely used Copy-Move and splicing forgeries.However,an image can contain one or more types of forgeries.This study has proposed a hybridmethod for classifying Copy-Move and splicing images using texture information of images in the spatial domain.Firstly,images are divided into equal blocks to get scale-invariant features.Weber law has been used for getting texture features,and finally,XGBOOST is used to classify both Copy-Move and splicing forgery.The proposed method classified three types of forgeries,i.e.,splicing,Copy-Move,and healthy.Benchmarked(CASIA 2.0,MICCF200)and RCMFD datasets are used for training and testing.On average,the proposed method achieved 97.3% accuracy on benchmarked datasets and 98.3% on RCMFD datasets by applying 10-fold cross-validation,which is far better than existing methods.

机体表面振动信号影响因素关联性分析

为了研究机体表面振动信号各影响因素的影响规律,在不同转速、转矩、润滑油温度及配缸间隙下,对比分析振动信号的峰值、方差、标准差及均方根等4个时域参数以及小波包分解得到的各频段能量的变化趋势。结果表明:随着转速的升高,燃烧压力峰值出现波动,在活塞惯性力的主导作用下,振动信号时域特征参数及频段5以上频率成分的能量呈增加的趋势;燃烧压力峰值随着转矩的增加而增大,振动信号时域特征参数及各频段能量均呈增加的趋势;随着润滑油温度的升高,在润滑油阻尼及燃烧压力的双重作用下,振动信号时域特征参数幅值整体呈降低的趋势,频段12以上频率成分的能量呈增加的趋势;随着配缸间隙的增加,密封性降低导致燃烧压力峰值减小,但由于活塞二次运动加剧,导致振动信号时域特征参数及频段5以上频率成分的能量呈现增加的趋势。

三维周期结构波阻板的带隙特性研究

波阻板(wave impeding block,简称WIB)常被用于动力机器、轨道交通、建筑施工等振源产生的振动污染控制。但波阻板受土层截止频率的制约,隔振频带窄且无法对特定频率范围进行针对性的振动控制,根据声子晶体,发展了一种三维周期结构波阻板(periodic structural WIB,简称PSWIB)。采用COMSOL有限元分别计算了散射体为正方体及球体时三维周期结构波阻板的带隙,讨论了结构、材料参数等因素对带隙特性的影响,并进行了正交试验优化设计。理论和数值计算均表明:三维有限周期结构波阻板所得衰减区与无限周期波阻板带隙范围一致,具有带隙性,振动衰减区内最大振幅衰减可达54 dB。与传统波阻板相比,三维周期结构波阻板拓宽了隔振频带,突破了截止频率的制约,并可依据振源特性设计三维周期结构波阻板材料参数满足对目标频率振动隔离的要求。

差分编码和块压缩的密文域可逆信息隐藏算法

随着数字信息与云存储技术的发展与成熟,密文域可逆信息隐藏算法正逐渐成为通信传输中数据隐私保护的研究热点。如何根据不同载体图像像素的分布特征,对局部区域内像素进行自适应识别编码,实现对载体更彻底的压缩以提升嵌入容量仍具有较大挑战。本文针对密文域可逆信息隐藏算法因载体图像冗余空间压缩不充分而导致嵌入容量较低的问题,提出一种基于差分编码和块压缩的密文域可逆信息隐藏算法。首先,根据自然图像局部区域内像素强相关性邻位作差,并基于块内最大差值对差值图像矩阵进行分类和自适应编码,同时设计分块置乱和块内像素扩散加密机制保证图像信息安全。然后,将自适应编码结果在对应的密文图像块上进行标记,压缩冗余空间。最后,通过位替换嵌入秘密信息。不同于其他算法,本算法对差分编码后的图像进行比特位重排列,从密文图像像素最低有效位开始,标记差值像素的符号位,其余各位面依次标记最小差值比特位。由于加密操作与自适应编码的可逆性,合法接收者可实现对原始明文图像的无损重构和秘密信息的无误提取。实验结果表明,与现有的几类算法相比,本文提出的算法具有更高的嵌入率和更好的安全性,在BOSSbase和BOWS-2两个数据集上的平均嵌入率达到3.027位/像素和2.937位/像素,在测试图像上平均嵌入率也均提高了0.57位/像素以上。

基于GPA+CBAM的域自适应水下目标检测方法

针对水下目标检测易出现域偏移而导致检测精度下降的现象,文中提出了基于图诱导原型对齐(GPA)的域自适应水下目标检测方法。该方法通过区域建议之间基于图的信息传播得到图像中的实例级特征,导出每个类别的原型表示用于类别级域对齐,从而聚合水下目标的不同模态信息,以此实现源域和目标域的对齐,减少域偏移带来的影响;同时添加了卷积块注意模块(CBAM),使神经网络能够专注于不同水域分布下的实例级特征。实验结果证明该方法能够有效提高发生域偏移时的检测精度。

Magmatic-tectonic response of the South China Craton to the Paleo-Pacific subduction during the Triassic:a new viewpoint based on Well NK-1

The Nansha Block(NB)is one of the blocks separated from the southern margin of the South China Craton(SCC)by the western Pacific subduction,which contains rich information of geodynamic and tectonic transformation.To reveal the essence of western Paleo-Pacific subduction during the Triassic period,Well NK-1 in this block was selected for petrographic study,and published research data from other cooperative teams were compared.A double-cycle pattern of basic to neutral magmatic volcanism was established,and 36 lithological rhythmic layers and representative cryptoexplosive breccia facies and welded tuff bands were identified.Combined with a reanalysis of published geochronological data,geochemical elements,and isotope geochemistry,we found that the rock assemblages could be divided into an intermediate-acid dacite(DA)series(SiO_(2)>65%)and basaltic(BA)series(Co<40μg/g),which was formed during the early Late Triassic((218.6±3.2)–(217.9±3.5)Ma).BA exhibits obvious calc-alkaline island-arc magmatic properties:(^(87)Sr/^(86)Sr)_i ratio ranging 0.70377–0.71118(average:0.70645),^(147)Sm/^(144)Nd ratio ranging 0.119–0.193(average:0.168),and chondrite-normalized rare earth element(REE)curves being flat,while DA exhibits remarkable characteristics of subducted island-arc andesitic magma:(^(87)Sr/^(86)Sr)_i ratio(0.70939–0.71129;average:0.71035),εNd(t)value(-6.2–-4.8;average:-5.6)andε_(Hf)(t)value(-2.9–-1.7,average:-2.2)show obvious crust-mantle mixing characteristics.BA and DA reveal typical characteristics of island-arc magma systems and typeⅡenriched mantle(EM-Ⅱ)magma.BA magma was likely resulted from the process whereby the continental crust frontal accretionary wedge was driven by the Paleo-Pacific slab subduction into the deep and began to melt,resulting in a large amount of melt(fluid)joined the asthenosphere on the side of the continental margin.In contrast,DA magma was likely resulted from the process whereby the plate front was forced to bend with increasing subduction distance,which triggered the upwelling of the asthenosphere near the continent and subsequently led to the partial melting of the lithospheric mantle and lower crust due to continuous underplating.The lithospheric thinning environment in the study area at the end of Triassic created suitable conditions for the separation between the NB and SCC,which provided an opportunity for the formation of the early intracontinental rift during the later expansion of the South China Sea(SCS).

边缘侧神经网络块粒度领域自适应技术研究

深度神经网络在边缘设备上运行时会面临模型缩放和域自适应2个挑战,现有的模型缩放技术和无监督在线域自适应技术存在缩放粒度粗、缩放空间小和在线域自适应时间长的问题。针对这2个挑战,提出一种块粒度的模型缩放和域自适应训练方法EdgeScaler,它包括离线和在线2个阶段。针对模型缩放挑战,离线阶段能够从各种DNN中检测和抽取块,并将其转换为多个派生块;在线阶段基于块和块之间的组合,提供大规模的缩放空间,解决模型缩放问题。针对域自适应挑战,设计了一种针对于块的残差Adapter,在离线阶段将其插入块中;在线阶段当新的目标域到来时,对所有的Adapter进行训练,解决块粒度缩放空间中所有选项的域自适应问题。在真实的边缘设备Jetson TX2上的测试结果表明,在提供大规模缩放选项的基础上,所提方法可以将域自适应训练时间平均减少85.14%,训练能耗平均减少84.1%。

基于Transformer块的混合域网络稀疏角度CT成像

目的 针对计算机断层扫描(Computed Tomography,CT)中由于不完全扫描数据导致图像噪声伪影严重的问题,提出一种基于Transformer块的混合域网络稀疏角度CT成像算法(Hybrid Domain network for sparse view CT imaging based on Transformer,HDTransformer)。方法 算法的主要思想是借助于新型的Transformer网络,构建适用于多阶段稀疏角度CT投影数据及图像数据的处理流,以提高稀疏角度CT图像重建质量;与现有两阶段混合域处理方法相比,本方法采用图像域-投影域-图像域三阶段混合处理流程,通过多阶段信息的联合互补提高成像质量;此外,针对不同阶段数据噪声伪影特点设计不同的Transformer块,以实现差异化的处理;更进一步,算法采用可微分的解析重建和投影运算,建立投影域与图像域数据的转换,最终实现端到端的稀疏角度CT优质成像流。结果 通过Mayo数据实验验证,其视觉结果表明:处理后的不同部位CT图像噪声伪影均能够得到较好的抑制;量化结果表明:处理后的CT图像峰值信噪比和特征相似性均优于对比方法。结论 实验的定性和定量结果表明:所提算法在去除图像伪影噪声方面要优于其他算法,具有更高的质量,验证了该方法的有效性。

中国大地构造单元划分

中国大地构造形成演化与大地构造分区研究已有百余年的历史,整体论述中国构造分区,都以不同学派对中国大陆地壳形成演化的不同认识论和方法论,有不同的方案。以黄汲清先生等多旋回构造观、王鸿祯先生等历史大地构造观和李春昱先生等板块构造观的"三大主流大地构造观"为指导思想的大地构造划分方案,是集中国地质构造之大成,在全国起指导作用,影响既广泛且深远。板块构造单元划分是当前板块构造细结构研究的关键问题。它既是板块构造研究的理论问题,也是区域地质研究和成矿预测评价亟待解决的实际问题。本文的大地构造分区图的编制是以地层划分和对比、沉积建造、火山岩建造、侵入岩浆活动、变质变形等地质记录为基础,承接融合中国"三大主流大地构造观"的经典划分理念,在板块构造—地球动力学理论指导下,以成矿规律和矿产能源预测的需求为基点,以不同规模相对稳定的古老陆块区和不同时期的造山系大地构造相环境时空结构分析为主线,以特定区域主构造事件形成的优势大地构造相的时空结构组成和存在状态为划分构造单元的基本原则,划分出中国的大地构造环境主要由陆块区和造山系组成为9个一级构造单元,以及相应的56个二级构造单元。中国大地构造研究还存在一系列重大科学问题,较准确地划分尚需很长时间的不懈努力。

中国大地构造阶段划分和演化

按照王鸿祯先生的地质构造演化阶段论和全球构造活动论的思路,遵循将今论古的比较构造地质学研究原则,以对接带、造山系和陆块区三类一级大地构造单元构造相的时空结构分析为主线,从超大陆汇聚与裂解不可逆演化和洋陆转换论的视角,认识理解中国大地构造时空结构组成特征,将中国大地构造划分为三个演化阶段。第一阶段：太古宙—前南华纪（〉820 Ma）。太古宙陆核形成（〉2 800 Ma）,新太古代原板块构造启动,洋陆分化,华北各陆块发育古弧-盆系统（2 800～2 500 Ma）,发育广泛的TTG片麻岩;古元古代（2 500～1 800 Ma）发育集宁、南辽河-荆山等弧盆系和嵩山裂谷、滹沱裂谷及华北基底形成（1 800 Ma）;中元古代—新元古代早期（820 Ma前）华北陆区在1.8Ga克拉通化后发育燕辽裂谷、熊耳—西洋河裂谷、渣尔泰—白云鄂博陆缘裂谷;扬子陆块和塔里木陆块区中元古代发育陆缘裂谷盆地,新元古代早期其周缘一系列弧盆系形成,扬子和塔里木基底形成,并参与罗迪尼亚超大陆汇聚过程。第二阶段：南华纪—中三叠世（820～227 Ma）,可分为5个构造期：（1）南华纪—震旦纪（820～541 Ma）构造期,罗迪尼超大陆裂解发育新元古代南华纪裂谷事件的火山-沉积岩及冰碛岩,古亚洲洋、原特提斯大洋及震旦大洋扩展,发育扬子、塔里木陆缘裂谷和裂陷盆地,华南洋萎缩为残余大洋。（2）寒武纪—中奥陶世（541～458 Ma）构造期,古亚洲洋、原特提斯洋持续扩张,中国西部一系列地块从扬子和塔里木大陆裂离,相应陆块均在伸展背景下形成被动大陆边缘,秦-祁-昆多岛弧盆系形成;印度陆块北部边缘形成寒武纪裂陷-裂谷盆地,上覆初始碳酸盐岩台地沉积（O1-2）。（3）晚奥陶世—志留纪（458～419 Ma）构造期,古亚洲大洋双向俯冲,向北俯冲制约阿尔泰-兴蒙多岛弧盆系形成,向南俯冲制约天山-准噶尔-北山多岛弧盆系形成及温都尔庙增生弧盆系发育;南天山大洋向北俯冲导致中天山岛弧形成;扬子、塔里木和印度等陆块的北缘均发育被动大陆边缘;志留纪震旦洋、华南洋消亡;塔里木、扬子与华北构成统一的泛华夏大陆,其西南缘秦祁昆造山系形成,在南东缘形成了华夏造山系。（4）泥盆纪—中二叠世（419～259 Ma）构造期,古亚洲洋、南天山洋萎缩消亡,天山-准噶尔-北山造山系和阿尔泰-兴蒙造山系形成（C2—P2）;华北陆块整体隆升（O3—C1）后,发育陆表海盆地;扬子陆块发育陆缘裂陷盆地。古特提斯大洋双向俯冲,向北俯冲制约北羌塘-三江多岛弧盆系发育,向南俯冲导致冈底斯陆缘弧形成（C—P）。（5）晚二叠世—中三叠世（259～227 Ma）构造期,中国西北盆-山构造格局定位;那丹哈达洋西向俯冲形成鹤岗陆缘弧。澜沧江弧后洋盆向东俯冲及金沙江-哀牢山弧后洋盆向西俯冲,昌都-思茅地块两侧形成陆缘弧。特提斯大洋向南俯冲导致冈底斯弧盆系形成。扬子区攀西裂谷形成,峨眉山玄武岩大规模喷溢。第三阶段：晚三叠世—新近纪演化阶段（227～2.6 Ma）。中生代时东部陆缘弧盆系形成;西北发育盆山构造;西南部喜马拉雅-冈底斯多岛弧盆系形成。新生代,中国东部沿海弧后裂陷及断陷盆地形成,印度-欧亚大陆碰撞,喜马拉雅-冈底斯造山系形成,中新世以来青藏高原强烈隆升。

佳木斯地块构造演化

佳木斯地块位于中亚造山带东段,是我国东北地区一个重要的大地构造单元,古生代以来经历了复杂的多构造体系叠合的演化过程。本文在总结近二十年已报导的相关研究成果基础上,结合笔者近年工作,探讨了佳木斯地块的基底属性和来源,重塑了佳木斯地块西缘碰撞拼贴,以及东缘俯冲-增生的构造演化过程。研究表明,佳木斯地块具有亲冈瓦纳大陆的构造属性,裂离后经历了长距离的北漂。与松辽地块先后两次拼合,首次发生于中志留世(~425Ma),在晚二叠世前后(~250Ma)沿原缝合带位置发生裂解,拉张出新的有限洋盆(牡丹江洋),并于侏罗纪(185~145Ma)与松辽地块沿牡丹江-依兰构造带再次碰撞拼贴,形成了高压变质的黑龙江增生杂岩带。而佳木斯地块东缘受晚石炭世-晚三叠世(305~250Ma)泛大洋的俯冲-增生事件影响,形成了跃进山增生杂岩,随后于中侏罗世-早白垩世(165~128Ma)在古太平洋板块的西向俯冲作用下,形成了饶河增生杂岩。因此,佳木斯地块的构造演化既涉及了晚古生代古亚洲洋构造域的消亡,又经历了中生代古太平洋构造域的叠加与改造,而黑龙江杂岩的形成标志着古太平洋构造体制与古亚洲洋构造体制的转换始于晚三叠世(~210Ma)。

基于分形压缩编码的数字水印技术

提出一种利用分形编码方案在图像中嵌入数字水印的方法。对数字图像分别进行传统分形编码和频域分形编码后 ,通过码书的比较 ,选择出一些R块 ,将这些块的编码方案更改 ,即用次优匹配D块替代最优匹配D块 ,从而实现数字水印的嵌入。实验证明该方案对图像质量几乎没有影响 ,在抗模糊、噪声干扰和剪切方面有较好的鲁棒性。

中蒙边界地区构造单元划分

以板块构造理论为指导,中蒙合作完成中蒙边界地区1∶100万地质编图成果的基础上,对中蒙边界地区构造格架进行了统一厘定和划分。该区Ⅰ级构造单元主体隶属于中亚构造带的阿尔泰—兴蒙造山系,部分属塔里木—华北陆块区。阿尔泰—兴蒙造山系可划分为10个Ⅱ级、27个Ⅲ级和69个Ⅳ级构造单元。塔里木—华北陆块部分划分出2个Ⅱ级、2个Ⅲ级和4个Ⅳ级构造单元。这些不同级别的构造单元较全面地概括了中蒙边界地区的地质面貌。

基于双域滤波的三维块匹配视频去噪算法

将双域滤波和三维块匹配算法相结合,充分利用了视频序列的时空频域的相关性,进行视频去噪。将三维块匹配视频去噪算法中小波阈值去噪得到的图像替换原引导图像,抑制了双域滤波算法基本层不平滑的问题。参考残差矩阵的能量谱对短时傅里叶变换系数进行阈值收缩,减少细节层的噪声残留。实验结果表明,本算法有效地解决了双域滤波算法的基本层不平滑、细节层有噪声残留的问题,主观和客观对比也表明,本算法有着较为优秀的去噪效果。