1.3 GHz 9-cell高性能超导腔高阶模耦合器电磁及热分析研究

中国科学院高能物理研究所于2023年6月完成了高品质因数1.3 GHz超导加速模组研发,在国际上率先实现了中温退火高品质因数超导腔模组技术路线。模组中集成了八只经过中温退火工艺处理的1.3 GHz9-cell超导腔,在模组的测试过程中超导腔的高阶模耦合器温升异常,导致超导腔无法在高梯度下稳定工作。通过HFSS软件和CST软件中的微波仿真模块对高阶模耦合器进行电磁分析,再通过理论和Ansys Workbench软件对高阶模耦合器进行热仿真分析,并结合模组的高功率实验,找到了超导腔性能异常的原因,并对超导腔高阶模耦合器的冷却方式进行了进一步的优化,解决了模组中超导腔高梯度下的不稳定性。

一株Clade1.3 ALV-J分离鉴定及其全基因组序列分析

为了解地方品种鸡禽白血病病毒(ALV)感染情况,本试验用从广西某养殖公司地方品种鸡采集的血浆样品接种DF-1细胞进行ALV的培养分离,然后用ALV-p27抗原检测试剂盒对其细胞培养上清进行ELISA检测,并进一步对细胞培养物进行病毒亚群的PCR鉴定和病毒分离株的全基因组序列测定与分析。结果显示:从鸡血浆样品中获得一株ALV,分离毒株经分子鉴定及测序分析确定其为J亚群(ALV-J),命名为GX22YL01;通过对毒株GX22YL01的全病毒基因组与参考毒株序列进行比对分析,发现其与课题组建立的ALV-J分类方法“Pilot tree”中的参考株GX14HG04相似性最高,且同处于Clade 1.3分支。

The Middle Miocene lobe-shaped and band-shaped submarine fans in the Lingshui Sag,Qiongdongnan Basin:source-to-sink system,genesis and implication

Deepwater oil and gas exploration is the key to sustainable breakthroughs in petroleum exploration worldwide.The Central Canyon gas field has confirmed the Lingshui Sag is a hydrocarbon-generating sag,and the deepwater reservoirs in the Lingshui Sag still have more fabulous oil and gas exploration potential.Based on drilling data and three-dimensional(3D)seismic data,this paper uses seismic facies analysis,seismic attribute analysis,and coherence slice analysis to identify the types of submarine fans(lobe-shaped and band-shaped submarine fans)that developed in the Lingshui Sag during the Middle Miocene,clarify the source-to-sink system of the submarine fans and discuss the genesis mechanism of the submarine fans.The results show that:(1)the deepwater source-to-sink system of the Lingshui Sag in the Middle Miocene mainly consisted of a“delta(sediment supply)-submarine canyon(sediment transport channel)-submarine fan(deepwater sediment sink)”association;(2)the main factor controlling the formation of the submarine fans developed in the Lingshui Sag was on the relative sea level decline;and(3)the bottom current reworked the lobe-shaped submarine fan that developed in the northern Lingshui Sag and formed the band-shaped submarine fan with a greater sand thickness.This paper aims to provide practical geological knowledge for subsequent petroleum exploration and development in the deepwater area of the Qiongdongnan Basin through a detailed analysis of the Middle Miocene submarine fan sedimentary system developed in the Lingshui Sag.

Genesis of the Jianbeigou Gold Deposit on the Southern Margin of the North China Craton: Insights from Fluid Inclusions, H-O-S Isotopes, and Pyrite in situ Trace Element Analyses

The Jianbeigou gold deposit is a typical lode gold deposit in the Qinling metallogenic belt, located on the southern margin of the North China Craton. Three stages of the hydrothermal process can be distinguished, including the quartz ± pyrite, quartz-polymetallic sulfide, and quartz-carbonate ± pyrite stages. From the early to late stages, the homogenization temperatures of primary fluid inclusions are 281–362°C, 227–331°C, and 149–261°C, respectively. The corresponding salinities estimated for these fluids are 3.9–9.9 wt%, 0.4–9.4 wt%, and 0.7–7.2 wt% Na Cl equiv. Combined with laser Raman spectroscopy data, the ore-forming fluid belongs to a H_(2)O-CO_(2)-Na Cl ± CH_4 system with medium–low temperature and salinity. The δ~(18)Ofluid and δD values for the quartz veins are-1.0‰ to 6.0‰ and-105‰ to-84‰, respectively, which indicates that the ore-forming fluid is of mixed source, mainly derived from magma, with a contribution from meteoric water. Pyrite has been identified into three generations based on mineral paragenetic sequencing, including Py1, Py2, and Py3. The pyrites have δ~(34)S sulfur isotopic compositions from three stages between 3.7‰ and 8.4‰, indicating that sulfur mainly originated from magma. Te, Bi, Sb, and Cu contents in pyrite were all high and showed a strong correlation with Au concentrations. Native gold and the Au-Ag-Bi telluride minerals were formed concurrently, and the As concentration was low and decoupled from the Au content. Therefore, Te, Bi, Sb and other low-melting point chalcophile elements play an important role for gold mineralization in arsenic-deficient ore-forming fluid. Combined with the geological setting, evolution of pyrite, and ore-fluids geochemistry, we propose that the Jianbeigou deposit can be classified as a magmatic–hydrothermal lode gold deposit. Gold mineralization on the southern margin of the North China Craton is related to Early Cretaceous magmatism and formed in an extensional setting.

一种基于多源数据的建筑物LoD1.3级三维模型快速构建方法

近年来,三维数字底座在城市空间监测和城市规划中的应用越来越广泛,如何快速构建大场景三维底座成为研究重点。本文研究了一种基于多源数据的建筑物LoD1.3级模型快速构建方法,通过建筑物DLG数据约束提取建筑物点云数据,计算顶部高程,基于DEM数据提取建筑物底部高程,基于DLG、底部高程、顶部高程进行三维拉伸建模,实现了城市大场景建筑物LoD1.3级模型快速构建。实验表明:本文构建0.8 km 2建筑物密集区LoD1.3级三维模型耗时56.11 s,三维模型高程中误差为2.19 m,且具备属性信息。本文提出的基于多源数据的建筑物LoD1.3级模型快速构建方法已在实景三维常州建设中得到应用,有效提升了全域建筑三维模型建设效率。

clade 1.3 J亚群禽白血病病毒与Ⅱ型禽网状内皮组织增殖病病毒共感染的病原分离鉴定及其囊膜基因分析

为了解已经开展禽白血病净化的广西地方鸡种瑶鸡中禽白血病病毒(Avian leukosis virus,ALV)与禽网状内皮组织增殖病病毒(Reticuloendotheliosis virus,REV)的感染情况,试验对鸡血浆样品接种的细胞培养物分别进行ALV群特异性抗原P27的ELISA检测和亚群特异性PCR鉴定,以及REV PCR鉴定。结果显示:一份样品为ALV-J和REV的混合感染,其中ALV-J命名为GX20YLJ1,REV命名为GX20YLR1;遗传进化分析显示,分离株GX20YLJ1和GX20YLR1分别属于clade 1.3的ALV-J和罕见的Ⅱ型REV;GX20YLJ1 gp37和GX20YLR1gp20亚单位的二级结构功能区由α-Helix组成,而GX20YLJ1 gp85和GX20YLR1 gp90亚单位的二级结构具有多样性;分离株GX20YLR1的gp90与美国REVⅡ型分离株SNV的gp90亚单位的二级结构最相似,与核苷酸序列分析的进化树结果一致。结果表明,广西地方品种净化鸡群仍存在clade 1.3的ALV-J,并首次发现与Ⅱ型REV的混合感染,提示在净化检测过程中要重视与REV等其他病原混合感染的检测,同时从基因及蛋白结构层的分析应更加关注gp85和gp90两个亚单位的遗传进化。

Nav1.3在神经病理性疼痛中的作用机制

Nav1.3是电压门控钠离子通道亚型之一,由SCN3A基因编码,对河豚毒素(tetrodotoxin,TTX)敏感。Nav1.3通道电流具有快速激活、快速失活和快速由失活状态恢复维持高频放电的特征,可在慢斜坡去极化期间被激活并产生持续钠电流,放大神经元兴奋性,在神经电信号的产生及传导过程中起着重要作用。研究发现Nav1.3的错义突变与部分神经损伤引起的电流变化具有共性,通过多种方式导致神经元异常放电,参与并调控痛觉过敏的发生。本文对Nav1.3参与神经病理性疼痛有关机制进行综述,探讨神经部位Nav1.3的表达变化与痛敏表型之间的关系、各种细胞因子及其受体调控Nav1.3的上下游信号及不同病理性疼痛变化差异的比较等,分析Nav1.3在神经病理性疼痛中的作用及其机制,探讨Nav1.3成为镇痛靶点的可能性。

1.3μm固体激光器研究进展

1.3μm波段固体激光器在多领域均有着重要作用,本文介绍了近20年来国内外不同晶体材料输出1.3μm波段激光的研究进展,包括几种常用的晶体如YAG、YVO_(4)、GdVO_(4)以及其他晶体。通过分析认为,对新材料、新机制的探索与应用是未来1.3μm波段激光器的主要发展方向。

Complex genesis of multiperiod fractures in the Middle Triassic Leikoupo Formation in the Pengzhou gas field, western Sichuan Basin, China

The cumulative expression of multistage deformation is complex multiperiod fractures,which are commonly seen in tectonic zones.The Middle Triassic Leikoupo Formation in the western Sichuan Basin Depression,China,is a typical marine carbonate reservoir with natural fractures caused mainly by tectonic movements.According to outcrops,drill cores,image logging,and fluid inclusions,the fracture characteristics,types of natural fractures,and interactions of fractures are determined.In total,419 natural fractures in 493.2 m of cores from 7 wells are investigated,which are mainly shear and tensile fractures with a small number of weathering generated fractures.Meanwhile,the results of the stable isotope analysis of δ13C and δ18O,as well as the flow fluid inclusion data,reveal four tectonic periods of fractures with different occurrences.Based on the history of regional tectonic evolution,indicating one period of weathering fractures ascribable to stratal uplift and three periods of structural fractures related to the sequential tectonic movements of the Longmenshan fault belt.By analyzing the interaction relationships of fractures,three types of fracture interaction relationships are observed:cutting,restraining,and overlapping.The four stages fractures are chronologically assigned to(1)the early Indosinian N-S trending compression,(2)the late Indosinian NW-SE compression,(3)the middle Yanshanian NE-SE compression,and(4)the early Himalayan E-W compression.The influence of natural fractures on gas migration and well production in marine carbonates is discussed,and indicates that tectonic fractures could provide seepage channels for gas migration and accumulation from near or distant hydrocarbon source rocks into the Middle Triassic Leikoupo Formation.This study utilizes a pragmatic approach for understanding the fracture genesis mechanism in oil and gas field with multiperiod fractures.

基于TLS1.3协议的智能电表安全设计

随着智能电网的发展,新旧设备共存,由于电表MCU主频及空间资源的限制,使得以纯软件方式实现加密算法耗时长,难以满足智能电表的通信需求。针对国外无硬件加密的智能电表需升级支持TLS1.3安全协议的需求,设计了一种TLS1.3协议的应用方案。基于电表响应时间要求,裁剪优化TLS1.3握手流程,结合加密套件及扩展协商的选择,保证电表安全强度的同时及时响应主站系统。通过设计证书预装方法,解决TLS1.3协议中证书认证无法应用于电网基础设施薄弱的地区等难题。通过厂内的批量测试及现场运行,证明了所设计的基于TLS1.3协议的通信安全方案在电表中运行稳定,无异常反馈。

The Relationship Between Indian Ocean SST and Tropical Cyclone Genesis Frequency over North Indian Ocean in May

Tropical cyclone(TC)activities in the North Indian Ocean(NIO)peak in May during the pre-monsoon period,but the TC frequency shows obvious inter-annual variations.By conducting statistical analysis and dynamic diagnosis of long-term data from 1948 to 2016,the relationship between the inter-annual variations of Indian Ocean SST and NIO TC genesis frequency in May is analyzed in this paper.Furthermore,the potential mechanism concerning the effect of SST anomaly on TC frequency is also investigated.The findings are as follows:1)there is a broadly consistent negative correlation between NIO TC frequency in May and SST in the Indian Ocean from March to May,with the key influencing area located in the southwestern Indian Ocean(SWIO);2)the anomalies of SST in SWIO(SWIO-SST)are closely related to a teleconnection pattern surrounding the Indian Ocean,which can significantly modulate the high-level divergence,mid-level vertical motion and other related environmental factors and ultimately influence the formation of TCs over the NIO;3)the increasing trend of SWIO-SST may play an essential role in the downward trend of NIO TC frequency over the past 69 years.

Genesis, metallogenic model, and prospecting prediction of the Nibao gold deposit in the Guizhou Province, China

Southwestern Guizhou province is one of China’s most important distribution areas of Carlin-type gold deposits. The Nibao deposit is a typical gold deposit in southwestern Guizhou. To elucidate the genesis of the Nibao gold deposit, establish a metallogenic model, and guide prospecting prediction, we systematically collected previously reported geological, geochemical, and dating data and discussed the genesis of the Nibao gold deposit,based on which we proposed the metallogenic model.Earlier works show that the Nibao anticline, F1 fault, and its hanging wall dragged anticline(Erlongqiangbao anticline) were formed before or simultaneously with gold mineralization, while F2, F3, and F4 faults postdate gold mineralization. Regional geophysical data showed extensive low resistivity anomaly areas near the SBT(the product of tectonic slippage and hydrothermal alteration)between the P2/P3 and the strata of the Longtan Formation in the SSE direction of Nibao anticline in the lower plate of F1 and hanging wall dragged anticline(Erlongqiangbao anticline), and the anomaly areas are distributed within the influence range of anticlines. Simultaneously, soil and structural geochemistry show that F1, Nibao anticline,Erlongqiangbao anticline, and their transition areas all show good metallogenic elements(Au, As, and S) assemblage anomalies, with good metallogenic space and prospecting possibilities. There are five main hypotheses about the source of ore-forming fluids and Au in the Nibao gold deposit:(1) related to the Emeishan mantle plume activity;(2) source from the Emeishan basalt;(3) metamorphic fluid mineralization;(4) basin fluid mineralization;(5) related to deep concealed magmatic rocks;of these, the mainstream understanding is the fifth speculation. It is acknowledged that the ore-forming fluids are hydrothermal fluids with medium–low temperature, high pressure, medium–low salinity, low density, low oxygen fugacity, weak acidity, weak reduction, and rich in CO_(2)and CH_(4). The fluid pressure is 2–96.54 MPa, corresponding to depths of 0.23–3.64 km. The dating results show that the metallogenic age is ~141 Ma, the extensional tectonic environment related to the westward subduction of the Pacific Plate. Based on the above explanation, the genetic model related to deep concealed magmatic rocks of the Nibao gold deposit is established, and favorable prospecting areas are outlined;this is of great significance for regional mineral exploration and studying the genesis of gold deposits.

Engineering Ferroelectric Interlayer between Li_(1.3)Al_(0.3)Ti_(1.7)(PO_(4))_(3)and Lithium Metal for Stable Solid-State Batteries Operating at Room Temperature

The poor contact and side reactions between Li_(1.3)Al_(0.3)Ti_(1.7)(PO_(4))_(3)(LATP)and lithium(Li)anode cause uneven Li plating and high interfacial impendence,which greatly hinder the practical application of LATP in high-energy density solid-state Li metal batteries.In this work,a multifunctional ferroelectric BaTiO_(3)(BTO)/poly(vinylidene fluoride-co-trifluoroethylene-co-chlorotrifluoroethylene)(P[VDF-TrFE-CTFE])composite interlayer(B-TERB)is constructed between LATP and Li metal anode,which not only suppresses the Li dendrite growth,but also improves the interfacial stability and maintains the intimate interfacial contact to significantly decrease the interfacial resistance by two orders of magnitude.The B-TERB interlayer generates a uniform electric field to induce a uniform and lateral Li deposition,and therefore avoids the side reactions between Li metal and LATP achieving excellent interface stability.As a result,the Li/LATP@B-TERB/Li symmetrical batteries can stably cycle for 1800 h at 0.2 mA cm^(-2)and 1000 h at 0.5 mA cm^(-2).The solid-state LiFePO_(4)/LATP@B-TERB/Li full batteries also exhibit excellent cycle performance for 250 cycles at 0.5 C and room temperature.This work proposes a novel strategy to design multifunctional ferroelectric interlayer between ceramic electrolytes and Li metal to enable stable room-temperature cycling performance.

A Scenario for Asymmetric Genesis of Matter

A previous preon scenario for the standard model particles, based on unbroken supersymmetry, is applied to the problem of matter-antimatter asymmetry. Attention is paid to the fact that the asymmetric hydrogen atom—like all atoms—can be described in terms of symmetric preons. Preons are created in the early universe. The matter-antimatter asymmetry is caused by stochastic correlations in charge density fluctuations of preons and antipreons and by the subsequent preon combinatorial mechanism to form quarks and leptons, and finally the three lightest elements. A tentative gravitino mass estimate is given based on minimal interference with nucleosynthesis. With local supersymmetry the scenario can be extended to supergravity.

新疆煤层气大规模高效勘探开发关键技术领域研究进展与突破方向

新疆煤层气资源量7.5万亿m^(3)(2000 m以浅),已施工煤层气井450口,年产气量达到0.8亿m^(3),新疆维吾尔自治区提出了2025年实现煤层气产量25亿m^(3)的目标,煤层气大规模高效开发成为紧迫的重大需求。从煤层气富集模式与选区技术、“甜点”预测探测技术、加速滚动开发与快速增储上产策略、地质适配性开发技术、煤层气与煤炭、油气协同开发技术5个关键技术领域,系统梳理了新疆煤层气勘探开发已取得的主要研究进展,分析提出了可能突破方向。研究表明:新疆煤储层具有多-厚煤层普遍、低阶煤发育、急倾斜煤层多见、煤体变形与构造控制显著、水文条件和露头条件复杂,和三“低”(含气量低、甲烷体积分数低、含气饱和度低)五“高”(高含气强度、高孔隙度、高地应力变化、高储层压力变化、高渗透率变化)的含气性及物性等煤层气地质独特性;煤层气成因与富集模式具有多样性,包括生物成因气、热成因气或生物-热复合成因及其相应富集模式,生物成因气藏或生物成因气贡献普遍;煤层气分布赋存规律呈现前陆盆地、山间盆地显著差异性;创新形成基于“两”分开(浅部与深部,低阶煤与中高阶煤)“两”结合(地质评价与工程评价,多元数据)的科学评价与基于“机器学习+三维地质建模”的精准选区技术是第1个突破方向。深部煤层气/煤系气“甜点”发育区域主要为盆内坳陷的凸起、盆内隆起的凹陷、盆缘斜坡,高产井位多为构造高点,发育层位为割理裂隙发育的原生结构煤层或孔裂隙发育的煤系砂砾岩储层;基于“地球物理+岩石物理+岩石力学地层新方法”和“地质甜点+工程甜点新理念”的深部煤层气/煤系气“甜点”预测探测技术是第2个突破方向。低风险、短周期、高效率、多批次工程部署是加速滚动开发的基本原则;中浅部煤层气快速增储上产技术策略是在优选新区块布井建井、对老区块煤层气井进行增产改造;深部煤层气快速增储上产技术策略是在大型盆地缓坡深部和盆内凸起“甜点”区优先部署开发;科学加速滚动开发与高效快速增储上产的工程部署方法与技术策略是第3个突破方向。在井网井型差异性优化部署、低储层伤害钻井固井、高可靠性录井测井试井、多井型高效分段压裂、低套压-控压排采管控等工程技术取得重要进展;发展构建新疆煤层气大规模高效勘探开发地质适配性技术体系是第4个突破方向。开展先采气后采煤、煤层气与煤共采、煤层气与原位富油煤共采,推动中浅部煤层气与煤炭协同勘探开发;开展煤系叠合型气藏开发、煤层气与煤系气共探共采、煤系全油气系统勘探开发,推动深部煤层气与油气协同勘探开发,已有关注和探索;煤层气与煤、油气共探共采是第5个突破方向。成果试图为新疆煤层气大规模高效勘探开发提供技术支持和工程决策参考。

多源点云优化的城市三维模型构建

简易模型与传统复杂的单体模型相比,对存储、可视化、传输和后续应用技术要求低,敏感信息承载量少,且能满足大部分应用需求,具有更高的应用价值。考虑应用需求与技术现状,自然资源部将城市三维模型(L0D1.3级)纳入实景三维中国建设任务中。目前相关生产以半自动化采集为主,工程化应用存在技术流程烦琐、效率较低且对数据量限制较大等问题。本文立足山东实际,提出了一种基于多源点云优化的城市三维模型快速构建技术,在充分利用现有数据基础上有效提升了数据处理效率,大幅减少了生产成本,并在实景三维山东建设过程中得到了有效验证,具有较好的社会经济效益与推广价值。

铜陵新桥层状菱铁矿成因的矿物学证据及成矿意义

安徽铜陵新桥矿区二叠系栖霞组底部和石炭系黄龙组—船山组之间产出层状、似层状菱铁矿矿层。开展菱铁矿矿层成因研究对于深入剖析区域层控矽卡岩型铜铁矿床成矿机制具有重要意义。本文利用粉晶X射线衍射(XRD)、扫描电镜(SEM)对菱铁矿矿石进行矿物学研究,结果发现菱铁矿矿石主要由菱铁矿、石英、伊利石和有机质等组成,菱铁矿颗粒粒径较小,表面具有成岩自生的自形石英硬模的微结构,SEM原位微区成分分析显示菱铁矿中除了主量元素铁,还含有大量的锰、锌和钙。矿石中存在两种微结构和不同成因的石英:表面具菱铁矿硬模和次生加大结构的碎屑石英;具六方双锥、单锥以及生物成因球形的自生石英。菱铁矿矿石的组成和矿物表面微结构表明其为沉积成因,非岩浆热液起源。富有机质和亚铁的沉积菱铁矿层和沉积胶状黄铁矿层协同作用,可能是铜陵地区乃至长江中下游成矿带层状铜铁矿床层控性重要制约因素,以及可能作为燕山期中酸岩浆演化的氧化性含铜成矿流体卸载成矿的地球化学还原障。

辽东矿集区大东沟金矿床成矿时代和成因:地质、年代学、地球化学和同位素制约

大东沟金矿位于华北克拉通北东缘辽东矿集区,矿体赋存于古元古代辽河群盖县岩组绢云千枚岩中,并与中生代石英闪长岩空间关系密切。为了深入揭示矿床成因与成矿地质背景,近期我们对其开展矿床地质、黄铁矿Re-Os和锆石U-Pb测年、成矿相关侵入岩的地球化学和Hf同位素以及硫化物S同位素工作。研究表明,其成矿可划分三期:第一期沉积成岩黄铁矿期(Ⅰ)、第二期为变质黄铁矿-毒砂期(Ⅱ)、第三期为热液期(Ⅲ)。其中,第三期又可划分黄铁矿-毒砂阶段(Ⅲ1)、多金属硫化物-石英阶段(Ⅲ2)和含黄铁矿石英-碳酸盐阶段(Ⅲ3)。热液期(Ⅲ)黄铁矿的Re-Os等时线年龄为130±18Ma(n=5,初始^(187)Os/^(188)Os=1.60±0.42),与成矿相关石英闪长岩的侵位年龄(133±1Ma)一致,指示金成矿作用发生在早白垩世。热液期Ⅲ1、Ⅲ2矿化阶段硫化物的δ^(34) S值为3.0‰~4.8‰,且明显不同于第一期沉积成因黄铁矿(8.9‰~10.2‰)和辽河群沉积-变质岩(7.0‰~23‰)的硫同位素组成,进一步揭示该矿床大规模成矿为岩浆热液作用形成,与石英闪长岩作用密切。石英闪长岩富集大离子亲石元素(Rb、Ba、U等),中度亏损高场强元素(Nb、Ta)、具有低的ε_(Hf)(t)值(-6.38~-2.82)以及弱氧化的属性;结合矿区内同期侵入岩数据,指示它起源于幔源镁铁质岩浆和壳源长英质岩浆的混合。结合区域地质资料,我们认为大东沟金矿床为中温热液型金矿床,成因上与同期弱氧化的闪长质岩浆有关,形成于早白垩世华北克拉通破坏峰期。

四川盆地三叠系气田型深层富钾锂卤水勘探历程、进展与展望

四川盆地三叠系嘉陵江组和雷口坡组不仅是常规天然气的主要赋存层位,同时也形成和储存了富含钾锂等关键元素的卤水资源。本文梳理总结了四川盆地三叠系气田型深层卤水勘探进程、成因机理、富集规律方面的进展和认识,并对潜在的研究重点进行了展望。四川盆地三叠系气田型深层卤水中钾、锂等关键金属元素均达到了工业品位,随着全球对锂资源需求的增大,由起初的“气钾兼探”逐渐向“气钾锂综合勘探”过渡。四川盆地三叠系深层富钾锂卤水的成因机制大体上相同,其中干旱气候条件下古海水的蒸发浓缩致使卤水中的钾锂富集;高温高压下含钾/锂元素的杂卤石/绿豆岩与埋藏卤水发生水岩反应,进一步促进了钾锂的富集;淋滤作用也是卤水中钾元素富集的重要成因。深层卤水主要储集于各类白云岩中,其富集主要受断裂、裂缝发育带和背斜等构造控制,富集规律可归纳为“孔隙裂缝储卤、断裂运卤、背斜核部富卤”。基于目前四川盆地气田型深层卤水的勘探现状和不足,未来应该加强地球物理勘探集成新技术的研发、资源评价方法与体系的优化、含高品位伴生元素新层系的勘探以及气田型卤水有效开发利用技术的研究。未来有望在四川盆地气田型深层卤水继续取得新的找矿突破。

山东栖霞大河崖金矿床包裹体特征研究及矿床成因初探

大河崖金矿床地处华北克拉通南缘的胶辽隆起区,栖霞—蓬莱金成矿带上,其空间产出受台前—陡崖断裂带和岩浆活动制约。为研究该矿床成矿流体特征及矿床成因,本文对其开展不同阶段的包裹体进行岩相学、显微测温、包裹体激光拉曼及S同位素分析。测试结果表明,包裹体可划分为Ⅰ型富液气液两相盐水包裹体、Ⅱ型含CO_(2)三相包裹体和Ⅲ型纯液相包裹体3类,矿石中的包裹体类型以气液二相包裹体和含CO_(2)三相包裹体为主。成矿期流体完全均一温度变化范围为216~298℃,盐度为3.71%~9.98%NaCleqv,密度为0.80~0.90 g/cm^(3)。成矿晚期流体完全均一温度变化范围为124~181℃,盐度2.41%~5.56%,密度0.91~0.98 g/cm^(3)。表明该矿床属于中低温、中低盐度、低密度的热液脉型矿床。从主成矿期(Ⅱ和Ⅲ阶段)到成矿晚期(Ⅳ阶段),成矿温度和盐度降低,成矿密度略有升高。矿石中黄铁矿δ^(34)S变化范围为+5.1‰~+6.51‰,与栖霞—蓬莱金成矿带其他金矿床基本一致。显示主要为岩浆硫,成矿物质可能来源于深部岩浆。根据流体包裹体及同位素研究并结合区域地质特征,大河崖金矿床的成矿与白垩世岩浆关系密切,受台前—陡崖断裂带控制,在其次级断裂形成沉淀富集成矿。