Metallogenic Systems on the Paleocontinental Margin of the North China Craton

The North China Craton (NCC) is one of the largest blocks composing the continent. Different types of continental margins well developed around the NCC, along with lots of metallogenic systems of different metals and different times. Based on the study on the structural evolution of the NCC, the authors made a new division of tectonic units of the NCC. Through an analysis of the data of 1:25000 geochemical survey on stream sediments, regional geochemical features of main ore-forming elements including Au, Ag, Cu, Pb, Zn, W, Ni, Co and Mo of the NCC are discussed in the paper. Then different metallogenic systems and their forming processes and geodynamics are discussed in detail. At last, temporal and spatial distribution regularities are summarized and ten favorable ore-control factors on the paleocontinental margins are put forward, including (1) abundance of ore sources; (2) rendezvous of ore-forming fluids; (3) high thermo-dynamic anomaly; (4) remarkable Earth crust-mantle interaction; (5) cluster of macroscopic structures and their long activities; (6) diversity of ore-forming environments; (7) long geohistory; (8) multiforms of critical transitional ore-forming mechanisms; (9) multi-staged and superimposed ore-formation; and (10) suitable preservation condition.

Tectonic Setting and Metallogenic System of North China Block Margins

The paleocontinental margins have frequent and intensive tectonic movement and various ore forming processes. According to their tectono dynamic characteristics, the paleocontinental margins can be classified into three types: the divergent, the convergent and the transformational. Each type has its specific geological geochemical processes and metallogenic system. The paper discusses the tectonic evolution and ore forming features of the North China block margins, puts forward conceptions such as complexity, variety and multi stage development of metallogenic evolution in the paleocontinental margins, and expounds five factors controlling the formation of large superlarge ore deposits in the paleocontinental margins: (1) channelway, (2) rendezvous of fluids, (3) abundance of ore source, (4) thermo dynamic anomaly, (5) long duration of structural activities.

Characteristics of the Composite Metallogenic System along the Jilin Paleocontinental Margin and the Evolution of Continental Dynamic Regimes

In view of the existing problems about the metallogenic epoch and origin of the complex along the Jilin paleocontinental margin, we propose the composite metallogenic system of the Jilin old land, based on the theory of metallogeny and from the continental dynamics and comprehensive analysis on the metallogenic characteristics. Its scientific theory is demonstrated by the following aspects: (1) Screening and analysis of the multi-stage super-imposition and sequences. The composite ore-forming system consists mainly of three types: the divergent-type epicontinental metallogenic system on the southern margin, the convergent-type epicontinental metallogenic system on the northern margin and the strike-slip-type epicontinental metallogenic system on the northeastern margin. Their major metallogenic epochs are Archean-Proterozoic, Variscan and Yanshanian respectively. (2) Comprehensive analysis of the genetic relations of the complicated deposits. The above-mentioned three types all indicate a consanguinity among granites, vein rocks and gold deposits, correspondence with geochemical elements, and unicity showing the same activities of mantle derived fluids and multi-source origin of ore-forming substances. (3) As to the mechanisms for mineral concentration, in addition to the sources, we also focus on the co-actions of permeability, vibration, gas-liquid state alternation and abrupt changes of flow velocity during the movement of ore-forming liquids, as well as the extraction and communication of multi-sequence circulating liquids. (4) It is helpful for establishing the relationship between metallogeny and the evolution of continental dynamic regimes, i.e., the ore-controlling correlations between the ore-forming elements-metallogenic series-metallogenic systems-composite metallogenic system and ore-controlling structural features (stratabound, primary and branching types)-regional faulting or secondary continental extension and collision-transformation of different continental dynamic types (divergent, convergent and strike-slip)-the evolution process of the whole old land for the Jilin old land margin. All these are helpful for further researches on the continental metallogenic dynamics.

STABILITY MARGIN OF SYSTEMS WITH MIXED UNCERTAINTIES UNDER THE IQC DESCRIPTIONS

Stability perturbation bounds problem for systems with mixed uncertainties is discussed. It is supposed that the linear part in the forward loop is of parametric uncertainties described by interval perturbation mode, and that the nonlinear part in the feedback loop is characterized by an integral quadratic constraint (IQC). The definition of stability margin under the interval perturbation mode is given by using the Minkowski functional. The infinite stability checking problem of the mixed uncertain system can be converted to finite or one dimensional stability checking for different structures of the IQC multipliers based on the concepts of biconvex and convex-concave junctions and their properties. The result is illustrated to be efficient through an example.

Characteristics of Paleoproterozoic Subduction System in Western Margin of Yangtze Plate

Paleoproterozoic subduction strongly occurred in the western margin of Yangtze plate. The basalticandesite volcanics of Ailaoshan Group and Dibadu Formation had been formed during paleo QinghaiTibet oceanic plate subduction under the paleoYangtze plate. Their trace element geochemistry suggests that their forming environments are continentalmarginarc and back arcbasin respectively. Consequently, the Paleoproterozoic subduction system in the western margin of Yangtze plate was established. Ailaoshan Group and Dibadu Formation came from an enriched mantle source that was contaminated by crustal sediments carried by subducted slab, and formed the Paleoroterozoic metamorphic basement of western margin of Yangtze plate. Ailaoshan Group is actually western boundary of Yangtze plate.

QUANTITATIVE METHODOLOGY FOR STABILITY ANALYSIS OF NONLINEAR ROTOR SYSTEMS

Rotor-bearings systems applied widely in industry are nonlinear dynamic systems of multi-degree-of-freedom. Modem concepts on design and maintenance call for quantitative stability analysis. Using trajectory based stability-preserving and dimensional-reduction, a quantitative stability analysis method for rotor systems is presented. At first, an n-dimensional nonlinear non-autonomous rotor system is decoupled into n subsystems after numerical integration. Each of them has only onedegree-of-freedom and contains time-varying parameters to represent all other state variables. In this way, n-dimensional trajectory is mapped into a set of one-dimensional trajectories. Dynamic central point （DCP） of a subsystem is then defined on the extended phase plane, namely, force-position plane. Characteristics of curves on the extended phase plane and the DCP＇s kinetic energy difference sequence for general motion in rotor systems are studied. The corresponding stability margins of trajectory are evaluated quantitatively. By means of the margin and its sensitivity analysis, the critical parameters of the period doubling bifurcation and the Hopf bifurcation in a flexible rotor supported by two short journal bearings with nonlinear suspensionare are determined.

Reactive Power Reserve Improvement Using Power Systems Inherent Structural Characteristics

This paper considers the use of the inherent structural characteristics of power system networks for improving the reactive power reserve margins for both topologically weak and strong networks. The inherent structural characteristics of the network are derived from the Schur complement of the partitioned Y-admittance matrix using circuit theory representations. Results show that topologically strong networks, operating close to the upper voltage limit could be made to increase their loadability margin by locating reactive power compensators close to generator sources, whereas topologically weak (ill conditioned) networks could be made to operate within the feasible operating limits by locating reactive power compensators on buses farther from generator sources.

Hilbert spectrum and intrinsic oscillation mode of dynamic response of a bilinear SDOF system: influence of harmonic excitation amplitude

Under harmonic wave excitation, the dynamic response of a bilinear SDOF system can be expressed by the Hilbert spectrum. The Hilbert spectrum can be formulated by (1) the inter-wave combination mechanism between the steady response and the transient response when the system behaves linearly, or (2) the intra-wave modulation mechanism embedded in one intrinsic mode function (IMF) component when the system behaves nonlinearly. The temporal variation of the instantaneous frequency of the IMF component is consistent with the system nonlinear behavior of yielding and unloading. As a thorough study of this fundamental structural dynamics problem, this article investigates the influence of the amplitude of the harmonic wave excitation on the Hilbert spectrum and the intrinsic oscillatory mode of the dynamic response of a bilinear SDOF system.

塔里木盆地西北缘乌什西次凹的地层系统和构造特征

乌什西次凹位于塔里木盆地西北缘,隶属于库车坳陷的乌什凹陷。它位于南天山主山脉(哈尔克山)和塔里木盆地柯坪—温宿凸起之间。区域构造格局上,这里是塔里木克拉通向西北自然延伸的部分。次凹北缘的阿合奇断裂是南天山造山带和塔里木克拉通的分界。乌什西次凹内发育与柯坪—温宿凸起相似的晚前寒武纪—古生代地层系统,包括寒武系、奥陶系和石炭系的烃源岩。新近系—第四系碎屑岩建造直接不整合于变形的古生代被动大陆边缘碎屑岩—碳酸盐岩沉积建造之上;剖面上,向南天山方向加厚,向塔里木克拉通方向减薄,呈现典型的前陆盆地剖面结构特征。这是一个晚新生代陆内前陆盆地,叠加在晚海西期—燕山期古隆起之上。这里的构造变形主要有3期,分别是中海西期、晚海西期—印支期和晚喜山期。变形以厚皮冲断构造及其相关褶皱为主,薄皮构造不发育。平面上,主构造线走向NE-SW。剖面上,以南天山向塔里木冲断为主。

新能源电力系统能量-灵活爬坡市场定价研究

新能源的零边际成本和间歇性出力为传统节点边际电价模型带来了新的挑战。“双随机”,特别是新能源供给的随机性会导致现货市场价格波动大,无法为市场参与者带来正确的价格信号。针对高比例新能源系统,提出了一种基于连续节点边际电价(continuous locational marginal pricing, CLMP)的出清机制的市场模型。首先计及了电力系统、储能系统和数据中心的运行约束,利用CLMP的定价机理构建了高比例新能源系统能量定价模型。然后考虑了发电机组与储能系统、数据中心提供运行灵活性爬坡服务,建立了高比例新能源电力系统能量-灵活爬坡市场协同定价模型。最后,算例测试定量分析了新能源渗透率与储能对系统电价的影响,量化了储能和数据中心的运行灵活性。

考虑用电和馈电模式的变流器电驱系统建模与稳定性分析

由大量异步电机驱动设备构成的电力电子化交流配用电系统存在严重的次/超同步振荡问题。电驱系统正常工作时具有用电和馈电2种运行模式,现场振荡现象表明不同的运行模式对系统的稳定性影响也不同。建立了含机侧系统的电驱系统详细阻抗模型,利用阻抗分析法揭示了电驱系统接入电网的次/超同步振荡机理,分析了运行模式、电网强度、控制参数、交流电压幅值等因素对系统次/超同步稳定性的影响,并基于相位裕度灵敏度明确了主导影响因素。基于实际系统数据,搭建了时域仿真模型,仿真复现了振荡现象,并验证了理论分析的正确性。

基于边际成本比较型竞价模式的电力现货市场机制设计

在建设新型电力系统、极端天气频发、一次能源价格飙涨、保供电常态化等背景下,文中提出了基于边际成本比较型竞价模式的电力现货市场机制,为统筹多市场主体利益、协调省间与省内交易提供了可行思路。首先,深度解析了现有电力现货市场机制在统筹多市场主体利益上面临的挑战,在采用边际成本比较型竞价模式的基础上,深入考虑不同类型发电机组的成本特性,提出了一种两阶段分层边际定价的电力现货市场机制,可有效统筹发电侧成本的可疏导性、用电侧电费的可负担性以及新能源机组的激励性。然后,提出了基于边际成本比较型竞价模式的省间-省内两级现货市场机制,并对其应用价值进行了探讨。最后,基于电力现货市场仿真平台开展算例分析,对所提市场机制的有效性和可行性进行了验证。

中国油气行业甲烷排放估算与减排分析

甲烷是仅次于二氧化碳的第二大温室气体,据统计全球甲烷排放中石油天然气行业排放占比高达三分之一,加强甲烷排放管控对推动“双碳”目标的实现具有重要的意义。为此,结合油气消费量预期、行业控排预期等,估算了2021—2060年中国油气行业甲烷排放量;并进一步分析了减排目标下技术减排潜力和减排成本,最后结合各类排放源占比及现有减排技术的成本效益,测算了2030年与2060年2个时间节点油气行业甲烷减排的边际成本。研究结果表明:①2021—2060年期间,油气行业甲烷排放量略有下降,天然气系统甲烷排放量增速变缓,其中运输和输配环节有较大减排潜力;②油气行业90%的甲烷排放量集中在30%的排放源中,有10%~20%的甲烷无法彻底通过技术减排;③在2030年、2060年实施的减排技术中,具有收益的技术比例分别达22.0%和44.4%;④2030、2060年的甲烷平均单位减排成本分别为22.33元/m^(3)和14.57元/m^(3)。结论认为,中国油气行业在中长期需要加快推进甲烷排放检测、报告、核查体系的建设,推动排放数据的精细化,并通过绿色金融、中国碳减排核证方法学开发等多种方式,持续提升行业甲烷减排积极性。

基于迁移学习的电力系统状态评估方法

随着可再生能源比例的增加和电网规模的不断扩大,电力系统的运行状态受不确定性因素的影响越来越大。以往研究中,以静态安全裕度为指标并考虑负荷延拓方向进行电力系统安全状态评估,未考虑在不同场景下或目标域数据集增大时的计算效率下降问题。因此,提出了一种基于迁移学习和卷积神经网络的电力系统安全状态评估方法。采用三层卷积层和三层池化层对所选取的负荷规律进行有效提取,并在不同场景下进行参数和权重迁移,实时快速掌握电力系统的运行状态。算例结果表明,该方法能在不同的场景保持较高的准确率,并且显著提高了计算效率。

基于中美战略博弈视角的资本市场做空机制比较研究

中美关系是当今世界上最为重要的国家间关系,值此百年未有之大变局,金融作为现代经济的制高点,近年来加剧竞争的大国博弈日益转向非传统的经济金融领域。自2021年以来,在美中概股不断遭遇市场做空,已严重影响我国的海外金融利益。本文通过分析中美博弈发展历程及演化机制,尤其是拜登政府执政以来的对华政策,比较研究了中美资本市场做空机制的做空主体、做空模式、监管制度、引发风险及其对我国的影响。本文研究为我国面对复杂多变的国际环境如何始终保持定力,有效应对美国对我国实施资本市场做空的持续打压提供理论支撑。

滨里海盆地石炭系储层综合分析与地质储量评估

滨里海盆地石炭系为碳酸盐岩地层,主要发育KT⁃Ⅰ与KT⁃Ⅱ两套含油层系,该区域分析化验资料较少,储层综合分析不全面,储量评估难度大。采用天然岩心,综合运用岩石薄片、高压压汞、孔渗分析等技术手段,对KT⁃Ⅰ与KT⁃Ⅱ层进行岩石学特征分析、储层物性及空间类型分析、储层渗流特征分析。综合分析结果表明:两套含油层系为典型的特低孔、特低渗储层,局部发育微裂缝,孔渗参数变化大,非均质性较强;KT⁃Ⅰ层渗流通道发育优于KT⁃Ⅱ层,根据渗流实验结果把两套储层划分为油气水三套系统的不同阶段。依据室内实验数据及测井解释成果进行储层识别与地质储量评估,单位面积(1 km^(2))地质储量为47.21×10^(4)t,单位面积(1 km^(2))注水开发可采储量为21.75×10^(4) t。该研究结果可为滨里海盆地石炭系储层油气资源评价及开发方案编制提供指导依据。

扬子地块北缘镇巴穿心店地区南华系碎屑锆石U-Pb年龄及其物源示踪

扬子地块北缘镇巴穿心店地区发育有完整的南华系—震旦系沉积地层,记录了研究区及邻区南华纪沉积特征,对于研究扬子地块北缘新元古代晚期构造演化历史和Rodinia超大陆演化过程具有重要的地质意义。研究区南华系由下至上可划分为4套岩石地层单位,分别为长安组、古城组、大塘坡组和南沱组。南华系砂岩地球化学特征表明,研究区南华系化学风化作用较弱,经历了较低程度的沉积物再旋回作用。砂岩的CIA、CIW、PIA、Rb/Sr等古气候指标显示,研究区南华系具有由寒冷干燥—有波动的寒冷干燥—趋于稳定的温暖湿润—寒冷干燥的古气候演化趋势。在Dickinson三角图解中清晰地反映了南华系各组砂岩具有再旋回造山带和切割岩浆弧物源的特征,同时砂岩岩石地球化学特征也指示南华系的物源区主体应由中酸性岩浆岩组成。南华系长安组、古城组和南沱组3件碎屑锆石U-Pb年龄样品的年龄分布特征类似,主要年龄区间为新元古代晚期(约780~约641 Ma),并显示出约750~约740 Ma的显著峰值。结合区域地质资料,研究区南华系沉积时代应为约720~约635 Ma,物源应主要来自位于现今研究区西侧的扬子地块北缘汉南—米仓山微地块的新元古代岩浆岩,其沉积事件对应于新元古代中晚期扬子地块北缘伸展-裂解阶段,为Rodinia超大陆裂解过程的沉积响应。

南海中等水深边际油田开发方案适用性分析

针对国内南海中等水深边际油田开发的需求,借鉴渤海及南海北部湾采用“蜜蜂模式”开发边际油田的工程经验,提出采用“水下生产系统+自升式生产储油平台或小型半潜式生产储油平台+DP穿梭油轮”的独立开发方案。通过对两种方案采油设施的功能、总布置及外输方案的介绍,表明在南海80~400 m的作业海域可根据不同水深条件选择适合的方案,实现边际油田滚动开发。为边际油田开发由浅水逐步向中深水挺进,提供新型低成本装备和高效开发模式。

陕南镇巴小洋坝地区南华系物源分析:来自碎屑锆石U-Pb年龄、碎屑成分分析及地球化学的证据

扬子板块北缘镇巴小洋坝地区出露了一套完整的南华纪沉积地层,分析其沉积时限、沉积环境及物源示踪对扬子板块北缘新元古代中晚期沉积-构造演化具有重要意义。本文对陕南镇巴小洋坝地区南华系砂岩样品进行碎屑锆石U-Pb测年分析,化学蚀变指数(CIA)、化学风化指数(CIW)、斜长石蚀变指数(PIA)、成分变异指数(ICV)判别及物源分析。结果显示小洋坝地区南华系的沉积时限应为720~635 Ma。长安组、古城组、南沱组沉积于寒冷干燥气候,而大塘坡组沉积于温暖湿润气候。其物源区主要为扬子板块北缘汉南—米仓山微地块。研究区南华系对应了新元古代中晚期扬子板块北缘地区的后碰撞-裂解阶段,是新元古代中晚期Rodinia超大陆裂解在该地区的沉积响应。

阻抗模裕度指标在新能源多馈入系统静态电压稳定评估的适应性分析

集中送出的新能源场站大多位于电网末端,随着其有功出力的增加,易出现静态电压失稳。该文将传统的阻抗模指标的应用对象由负荷推广至新能源场站,丰富了该指标在静态电压稳定评估方面的适用性场景,包括含无功补偿的新能源系统、新能源集群馈入系统、以及新能源多机多馈入系统。具体地,首先,分析新能源单馈入系统的临界静态电压稳定条件,并据此给出用于评估新能源场站静态电压稳定性的阻抗模裕度指标及稳定判据;其次,通过将无功补偿设备并入系统阻抗,分析无功补偿对于指标的影响;再次,证明在新能源的集群馈入系统中,公共耦合点(point of common coupling,PCC)的电压失稳将发生在单个新能源场站之前,并据此确定PCC点作为指标的计算节点;之后,为考虑多机多馈入系统中不同新能源场站间的影响,在指标的计算过程中,保留待评估的关键新能源场站,将其他新能源场站等值为阻抗,并入节点阻抗矩阵中,实现方法在多机多馈入系统中的扩展应用。最后,基于PSD-BPA中建立的单机单馈入系统、多机多馈入系统、以及某省实际大电网算例验证指标的有效性。