The Features of Sedimentary Facies and Copper Enrichment Metallogenic Regularities of Kuzigongsu Group in Sareke Glutenite Type Copper Deposits,Wuqia,Xinjiang

1 Introduction Sareke glutenite-type copper deposit is the large size copper deposit discovered in recent years,and it is located Sarekebayi intracontinental pull-apart basin in the western margin of the Tarim basin.Conglomerate of

A Discrete-type Continuation Regularization Method and its Application

Discrete-type continuation method for solving nonlinear system of equations and Tikhonov's regularization method for solving linear ill-posed problems are combined into a stable and widely convergent one for solving nonlinear operator equations with difficultly computed and ill-conditioned derivatives. Some results about their convergence are given The application of this method to solve the inverse problem of one-dimensional diffusion equation is demonstrated.

A Preliminary Review of Metallogenic Regularity of Copper Deposits in China

Copper resources in China are rich, but imported copper products are still required. Researches on metallogenic regularity of major types of copper deposits by geologists have involved in worldwide classification, significant copper belts, representative copper deposits, etc. Studies on metallogenic regularity of copper deposits in China also have made achievements with a long-term work. Combined with latest exploration advances obtained in recent ten years, this review aims to conclude the achievements of researches on copper metallogenic regularity in China. Based on data of 814 copper deposits and other ore （mineralized） occurrences, ten prediction types of copper deposits have been suggested. Porphyry and skarn copper ores are taken as the key targets. Porphyry copper deposits are the most important one which concentrate in Gangdese, Changdu-Sanjiang, Dexing and East Tianshan. The Cenozoic and Mesozoic are the major metallogenic epochs. Four main metallogenic epochs are been studied based on the copper ore geochronological data including Precambrian Era （Archean and Proterozoic）, Paleozoic Era, Mesozoic Era and Cenozoic Era. Based on the study of metallogenic series of ore deposits in China, twenty-seven metallogenic series of copper deposits are proposed. This is suggested to deepen the study of metallogenic regularity of copper ore and provide the theory guide for copper resources prediction in China.

Outline of Uranium Resources Characteristics and Metallogenetic Regularity in China

Uranium,as one of twenty-six kinds of important minerals in China,is strategic resource and energy mineral,which has been thoroughly investigated in the project of National Potential Evaluation of Uranium Resource.During the implementation of this project,the authors summarized the metallogenic regularity of uranium resource in China systematically,through the researches of geological characteristics of uranium resource,uranium deposits type（genetic and prediction type）,temporal and spatial distribution,and metallogenic series.Based on the investigation of present situation and progress in uranium exploration,this paper proposes the uranium deposits in China should be divided into 4 classes,9 types,21 subtypes in genetic,and 50 types in prediction;suggests to divide China into 29 uranium metallogenic belts and 20 uranium prospective area,and constructs 20uranium-polymetallic metallogenic series,through summarizing temporal and spatial distribution characteristics and metallogenic regularity of uranium deposits in China.The above research is beneficial to the comprehensive understanding of regional uranium metallogenic regularity,and will direct the uranium exploration in the future.

东北地区金矿成矿规律及找矿方向

金矿是一种重要的贵金属矿产,也是东北地区优势矿产之一。东北地区金矿资源丰富,分布具有明显的区域性集中趋势,是我国岩金尤其是砂金的重要产区。本文系统收集和整理了已有东北地区金矿地质资料,全面总结了东北地区金矿资源禀赋、矿床类型、时空分布规律、成矿演化,指出了进一步的找矿方向。综合金矿床的工业类型和成因类型,将东北地区金矿床分为砂矿型、岩浆热液型、陆相火山岩型、变成型和受变质型、斑岩型、叠加型及成因暂时未查明的流体型等类型。岩金主要分布于华北成矿省辽东成矿带、华北陆块北缘东段成矿带,吉黑成矿省小兴安岭—张广才岭成矿带、吉中—延边成矿带,大兴安岭成矿省东乌珠穆沁旗—嫩江成矿带等;而砂金主要分布于黑龙江省三江沿岸,大兴安岭成矿省东乌珠穆沁旗—嫩江成矿带、吉黑成矿省佳木斯—兴凯成矿带、小兴安岭—张广才岭成矿带等。东北金矿具有多旋回、多期次成矿的特点,按其规律可划为太古宙、元古宙、加里东期、华力西期、印支期、燕山期、喜马拉雅期等7个成矿期。划分了13个成矿系列,22个成矿亚系列,22个三级预测区,显示出良好的成矿条件和找矿前景。

The Metallogenetic Regularities of Lithium Deposits in China

Lithium resources support the development of high-technology industries. China has abundant lithium resources which are mainly distributed in Tibet, Qinghai, Sichuan and Jiangxi. Salt lakes in China have significant lithium reserves, but lithium is mainly produced from hard rock lithium deposits because the extraction from salt lakes requires further improvements. The hard rock lithium deposits mainly occur in granitic pegmatite in the Altay region of Xinjiang and the Jiajika deposit in western Sichuan Province; they mainly formed in the Mesozoic and occurred in a relatively stable stage during orogenic processes. On the basis of the information from 151 lithium deposits or spots, 14 lithium metallogenic series were identified, and granitic pegmatite, granite, and sedimentary types were considered to be the main prediction types of lithium resources. Twelve lithium mineralization belts were divided and a series of maps showing the lithium metallogenetic regularity in China were drawn. We conclude that the hard rock and brine type of lithium resources possibly have a similar lithium source related to magmatism. The mctallogenic features of the lithium in China were related with the distinct history of tectonic-magmatic activity in China. This study benefits the assessment of, and prospecting for, lithium resources in China.

ITERATIVE REGULARIZATION METHODS FOR NONLINEAR ILL-POSED OPERATOR EQUATIONS WITH M-ACCRETIVE MAPPINGS IN BANACH SPACES

In this paper, a modified Newton type iterative method is considered for ap- proximately solving ill-posed nonlinear operator equations involving m-accretive mappings in Banach space. Convergence rate of the method is obtained based on an a priori choice of the regularization parameter. Our analysis is not based on the sequential continuity of the normalized duality mapping.

POLYGENETIC COMPOUND ORE DEPOSITS AND THEIR ORIGIN IN THE CONTEXT OF REGULARITIES IN CRUSTAL EVOLUTION

Polygenetic compound ore deposits are here defined as those ore deposits which evidently possess n1any sided genetic characteristics as a comprehensive result of more than one rnineralization stages, from many rnaterial sources, and of many genetic types. They are formed most commonly during the diwa (geo(lepression) stage in the process of crustal evolution and, therefore, spread most widely in diwa regions. At the present stage of our knowledge, they may be subdivided into three principal models and many types of metallogenesis, controlled by different geotectonic conditions and being distributed in time and in space according to the corresponding regularities. This is a newly rccognizcd, third gcnetic type of ore deposits, being not reasonable to be simply referred to either pure endogenic or pure exogenic origin. They are very important and are of great study significance, becausc they comrnonly are rich and have a large amount of reserve with high economic value.

Co-regular集上的可计算算子

Co-regular热集是Rd上的一类集合,在第二类能行性理论(简称TTE)的框架下,研究co-regular集组成的类P上若干算子的可计算性,这些算子主要包括交、并、象、原象、补集的内部运算和开集的co-regularization等.结果表明,此前提出的所有不等价表示式中,只有个别表示式对这些算子是可计算的.

Co-regular集的可计算性探讨

引入了在TTE框架下,利用开集和闭集的表示式,定义了度量空间中co-regular集的若干不等价表示式;并对这些表示式的强弱关系进行了论证。研究表明:这些表示式的强弱,有一个明确的顺序;在被引入的不等价表示式中,η:=θ<∧ψ>是co-regular集所有表示式中最强的。

A Preliminary Review of the Metallogenic Regularity of Nickel Deposits in China

The nickel deposits mainly distributed in 19 provinces and autonomous regions in China are 339 ore deposits/occurrences, including 4 super large-scale deposits, 14 large-scale deposits, 26 middle- scale deposits, 75 small-scale deposits, and 220 mineralized occurrences. The prediction types of mineral resources of nickel deposits are magmatic type, marine sedimentary type and regolith type. The formation age is from the Neoarchean to the Cenozoic with two peaks in the Neoproterozoic and the late Paleozoic. The nickel deposits formed in the Neoproterozoic are located on the margin of the North China Block and Yangtze Block, and those formed in the late Paleozoic are mainly distributed in the Central Asian Orogenic Belt （CAOB）, Emeishan and the Tarim Large Igneous Provinces （LIPs）. Magmatic nickel deposits are mainly related with broken-up continental margin, post-collision extension of the orogenic belt and mantle plume. According to different tectonic backgrounds and main characteristics of magmatism, the Ni-Cu-Co-PGE metallogenie series types of ore deposits related with mantle-derived mafic-ultramafic rocks can be divided into 4 subtypes： （1） the Ni-Cu-Co- PGE metallogenic series subtype of ore deposits related with mantle-derived mafic-ultramafic rocks in the broken-up continental margin, （2） the Ni-Cu-Co-PGE metallogenic series subtype of ore deposits related with mantle-derived mafic-ultramafic rocks in mantle plume magmatism, （3） the Ni-Cu-Co- PGE metallogenic series subtype of ore deposits related with mantle-derived mafic-ultramafic rocks in the subduction of the orogenic belt, and （4） the Ni-Cu-Co-PGE metallogenic series subtype of ore deposits related with mantle-derived mafic-ultramafic rocks in post-collision extension of the orogenic belt. We have discussed in this paper the typical characteristics and metaliogenic models for Neoproterozoic Ni-Cu-（PGE） deposits related with broken-up continental margin, Cambrian marine sedimentary Ni-Mo-V deposits related with black shale, early Permian Ni-Cu deposits related with post-collision extension of the orogenic belt, late Permian Ni-Cu-（PGE） deposits related with Large Igneous Provinces （LIPs）, and Cenozoic Ni-Au deposits related with regolith. The broken-up continental margin, mantle plume and post-collision extension of the orogenic belt are important ore- forming geological backgrounds, and the discordogenic fault, mafic-ultramafic intrusion, high MgO primitive magma （high-MgO basaltic magma）, deep magmatism, sulfur saturation and sulfide segregation are 6 important geological conditions for the magmatic nickel deposits.

A Preliminary Review of Metallogenic Regularity of Tungsten Deposits in China

Tungsten ore resources are abundant in China with relatively complete types of deposits. Skarn type and quartz vein type deposits are dominated in the tungsten resources, whereas quartz vein type wolframite deposits are most important in terms of exploitation and utilization. Skarn type tungsten deposits are concentratedly distributed in the central Nanling region, such as South Hunan, South Anhui and the eastern Qinling region, while quartz vein type tungsten deposits occur mainly in South China, such as West Fujian, South Jiangxi, North Guangdong and South Hunan. The most important metallogenic epoch of tungsten is the Mesozoic, while the metallogenic tectonic setting is featured by an intracontinental environment after orogeny with sever tectonic movements, deep-seated faults and frequent magmatic activities, especially Mesozoic granitoids closely related to tungsten-tin mineralization. 22 metallogenic series of ore deposits characterized by or significantly related to tungsten were defined based on precise statistic information of 1199 tungsten mining areas and thorough the summary of metallogenic regularities. Based on studies of the metallogenic regularity of tungsten deposits, skarn type （or greisen type）, quartz vein type and massif-type of tungsten deposits are thought to be the key prediction types. 65 tungsten-forming belts and 22 key ore concentration areas were ascertained and a distribution map of tungsten-forming belts of China was compiled, which provided a theoretical basis for evaluation and prediction of potential tungsten resources.

A Preliminary Review of Metallogenic Regularity of Gold Deposits in China

Gold is one of the most important mineral resources in China with its rich mineral resources. In recent years, significant progress has been made on the process of gold resource exploration. Some large and giant gold deposits were newly found and some important expansions in the main mining regions were also been completed. Studies on metailogenic regularity of gold deposits in China also have made achievements with a long-term work. This review aims to conclude the achievements of research on gold metallogenic regularity in China. Based on the data of about 2000 gold deposits and other ore （mineralized） occurrences, gold deposits in China were classified into five prediction types： gold deposits genetically related to granite-greenstone formation, gold deposits related to sedimentary formation （including the Carlin type and the metamorphosed clastic rock related vein gold deposit）, gold deposits genetically related to volcanic rocks （including the continental and marine types）, gold deposits genetically related to intrusions （including the porphyry type and the inner intrusion and contact zone related gold deposit）, gold deposits of supergenesis （including fracture zone-altered rock gold deposit, placer gold deposit, gossan type gold precise chronology data of gold deposits indicate deposit and soil type gold deposit）. Statistics on that there occurred 5 main periods of gold- mineralization in geological history of China. They were Neoarchean to Paleoproterozoic, Meso- Neoproterozoic, Paleozoic, Mesozoic, and Cenozoic. Gold deposits in China mainly formed in the Mesozoic and the Cenozoic. On the studies of the spatial-temporal distribution characteristics of gold deposits, 53 gold-forming belts were delineated in China. The metallogenic regularity of gold deposits was preliminarily summarized and 71 gold metallogenic series were proposed in China. This suggests that it is necceary to deepen the study on metallogenic regularity of gold deposits and to provide the theory guide for the ore-prospecting for gold resources in China.

吉黑东部地区金矿资源禀赋及成矿规律特征

金矿是吉黑东部地区的优势矿种之一,资源丰富、类型多样.通过系统收集和整理已有金矿地质资料,全面总结了吉黑东部地区金矿资源禀赋、矿床类型、控矿因素、时空分布规律、成矿演化及资源潜力,将研究区金矿床划分为6种成因类型、48个主要预测类型和5个成矿期.研究区金矿主要产出于经历多期次构造运动和频繁岩浆活动的活动大陆边缘和岛弧(火山弧)等构造单元内,特别是华力西期—燕山期大规模的构造、岩浆活动是金矿床形成的重要控制因素.通过总结上述成果,在研究区划分出34处金矿重要找矿远景区,明确了研究区金资源潜力和找矿方向,并提出加强重要找矿远景区及已知矿床深边部和外围金矿资源勘查是实现找矿突破的重要途径.

利用点电流源和Tikhonov正则化的潜艇稳恒电场反演方法

为了评估潜艇水下腐蚀相关稳恒电场分布特性,从潜艇水下腐蚀相关稳恒电场产生机理出发,基于等效点电流源建立潜艇水下腐蚀相关稳恒电场正演模型,并利用Tikhonov正则化根据已知电场数据求解等效点电流源电流强度,对潜艇周围海水空间的腐蚀相关稳恒电场进行推算。将某型潜艇的COMSOL软件仿真结果作为模拟试验数据,对所提方法有效性进行验证。结果表明:由水深38 m电场值向水深42.5 m和水深33.5 m进行反演时,相对均方根误差、最大值相对误差、峰峰值相对误差均不超过0.06;由较近平面向较远平面进行反演时,即使推算深度达到45 m,相对均方根误差仍然在0.21以内;噪声标准差为实际电场最大值的0.1倍时,反演误差仍然小于0.1。该算法抗噪声能力强,精度较高,能较好地用于工程实践。

云南省锗矿资源成矿规律概要

锗(Ge)矿是我国的战略矿种,也是云南省优势矿产。云南已探明Ge资源储量大,开发利用程度高,找矿空间大,主要包括煤层型和碳酸盐岩容矿型两类矿床。其中,煤层型锗矿床主要分布在滇西腾冲、芒市、沧源、临沧、澜沧等地,形成时代相对集中,为新近纪;碳酸盐岩容矿型锗矿床主要分布在滇东北东川、会泽、彝良、鲁甸等地,与铅锌矿床同体共生,形成时代普遍认为是三叠纪。本文全面梳理这两类矿床的成矿地质条件和资源空间分布特征,总结了其成矿规律;综合圈定出找矿预测区共23处。由此提出,当前应加强现有Ge矿床深部和外围地区接替资源找探矿及综合回收利用研究,及时对找矿预测区和有利远景区进行找矿勘查与靶区优选工作,尽快实现老区资源增储和新区找矿突破,为打造世界级Ge资源产业基地和国家Ge矿资源战略储备需求提供资源和技术保障。

龙陵县新寨-茅草园稀土矿特征及控矿条件浅析

龙陵新寨-茅草园地区花岗岩风化壳离子吸附型稀土矿床受内生地质和表生地质条件双重控制,主要赋存于白垩纪花岗岩体全风化层中下部及强风化层上部,V 1-1矿体分布面积38.59km 2,单工程控制矿体品位(SREO)0.035%~0.128%,平均0.047%;V 1-2矿体分布面积16.85 km 2,单工程控制矿体品位(SREO)0.035%~0.110%,平均0.048%,达大型远景规模,具有较好的勘查开发前景。

云南开远市吉德金矿地质特征及成矿模式

吉德金矿矿体主要呈似层状、透镜状产于峨眉山玄武岩与下伏灰岩岩溶不整合面、玄武质火山碎屑岩夹层及次级构造破碎带中,有红土型和岩溶角砾岩型两种类型,金以微粒自然金为主,目前矿床规模较小、地质研究程度较低。通过总结成矿规律、构建成矿模式,对矿区及外围寻找红土型和岩溶角砾岩型金矿具有指导作用。

柴达木盆地与周缘铀矿特征及砂岩型铀矿找矿方向分析

铀是中国的关键性能源金属和战略矿产资源之一。柴达木盆地与周缘虽然取得了一些铀矿找矿成果,但与之广袤的面积相比仍显不足。在简要介绍柴达木盆地区域铀矿地质背景的基础上,整理并分析了该区典型铀矿床(点)特征和主要中酸性岩浆岩的Th、U含量及锆石U Pb年龄数据等资料。结果表明,柴达木盆地与周缘铀矿化类型多样、种类齐全,主要为碱性岩(脉)型、花岗伟晶岩型、花岗岩(内带、外带、碱交代)型、火山岩型、层间氧化砂岩型、层间氧化油气还原砂岩型等。柴达木盆地与周缘“全位”铀成矿模式涵盖了该区可能存在的16种铀矿化类型。铀成矿时代从加里东晚期(436~401 Ma)直至现代。柴达木盆地北缘、南阿尔金和东昆仑构造带在区域地质演化和铀成矿作用的时间上具有一定的一致性,但是由于构造带的抬升剥蚀差异,柴北缘富铀岩浆岩和铀矿化保存最好,其次为南阿尔金,最差的是东昆仑构造带。结合盆缘成矿物质(源)、成矿流体场(运)、山前成矿空间(储)、盆内还原障(保)等成矿条件分析,指出柴达木盆地北部以侏罗系为目标层位的层间氧化砂岩型铀矿远景区有5个,南部和西部以新近系与更新统为目标层位的层间氧化油气还原砂岩型铀矿远景区有6个。

金银花胡萝卜微管蚜发生规律及防治适期研究

目的:明确金银花胡萝卜微管蚜越冬卵和春季发生蚜型的形态特征和发生规律。方法:2022年2月,在田间观察胡萝卜微管蚜越冬卵分布部位,采集虫卵及各蚜型成虫,室内镜检并描述其形态特征;2022年3—6月,在金银花田按五点取样法选取植株,定期调查各蚜型数量,采用最优分割法划分胡萝卜微管蚜种群动态并分析其与金银花物候的关系。结果:胡萝卜微管蚜虫卵主要分布在金银花植株的芽鳞、树杈和树皮缝等部位。胡萝卜微管蚜春季在金银花上依次发生干母、无翅孤雌蚜和有翅孤雌蚜3个蚜型,其中干母主要发生于3月9日至4月7日,高峰虫量为29.4只/梢;无翅孤雌蚜和有翅孤雌蚜在3月28日至5月27日混合发生,分别于4月19日和5月13日到达高峰,峰值分别为75.5只/梢和105.6只/梢。胡萝卜微管蚜种群动态与金银花物候特征密切相关,在金银花萌芽展叶期,蚜虫种群处于初建期和缓慢增长期,种群数量低,最高虫量为29.4只/梢;金银花抽梢期,蚜虫种群处于快速增长期,数量迅速上升;金银花花蕾期,蚜虫种群处于高峰期,数量达到高峰值,为370.5只/梢;在金银花开花期,蚜虫种群处于衰退期,数量迅速下降,至6月初基本消失。结论:金银花越冬期是防控胡萝卜微管蚜虫卵的关键期,萌芽展叶期是防控该蚜虫春季种群爆发的关键期。