哈萨克斯坦旅华客源市场特征与拓展分析     

席宇斌  赵倩 《世界地理研究》2016,(3):125-132

自中国与哈萨克斯坦建交以来,双方逐渐深化和拓展合作领域。两国推进中方丝绸之路经济带建设同哈方"光明之路"新经济政策的对接,更加注重旅游等人文交流合作领域。因此,研究哈萨克斯坦旅华客源市场具有十分重要的现实意义。本文以连续多年的统计数据为基础,研究哈萨克斯坦游客的入境旅游优势,并从历史发展阶段、人口统计学特征、人均消费与平均停留时间、人均消费构成、入境方式、年内时间分布规律、在华空间分布和出境流向等八个方面分析哈萨克斯坦旅华客源市场特征,并得出相应结论。文章最后从创新旅游合作领域、丰富游客入境条件和进行旅游宣传推广三方面为两国市场拓展提出建议。  相似文献   

哈萨克斯坦环巴尔喀什斑岩铜矿地质与成矿背景研究   总被引：28，自引：18，他引：10  

李光明  秦克章  李金祥 《岩石学报》2008,24(12):2679-2700

中哈萨克斯坦位于中亚造山带中部,是中亚型造山带及中亚斑岩铜矿成矿域的重要组成部分,已发现数十个大型和超大型矿床,成群成带分布。主要的斑岩铜矿类型有斑岩铜-金矿、斑岩铜矿、斑岩铜钼矿,大多具同期火山岩。已建立的热液蚀变分带模式具有碱性蚀变和酸性蚀变两个阶段,已有的硫铅同位素数据表明成矿物质来源于深部。该地区的斑岩铜矿形成与多阶段构造演化有关,早古生代的斑岩铜矿与岛弧演化的早阶段有关,而晚古生代的斑岩铜矿与泥盆纪火山—岩浆弧、石炭纪—二叠纪的火山—岩浆弧有关。从中哈萨克斯坦的北西向南东方向,斑岩铜矿的形成时代逐渐变年轻。虽然经过数十年的研究,但该地区的有关斑岩铜矿的精细时空结构仍未建立。因此,含矿斑岩体与蚀变矿化年龄的精确测定、区域成矿地球动力学背景及其演化、斑岩铜矿的精细时空结构、与中国邻区的构造—岩浆—成矿带的连接对比将是以后的研究方向。  相似文献   

哈萨克斯坦古河道砂岩型S铀矿床成矿特征   总被引：2，自引：0，他引：2  

姚振凯  陈为义  杨志  马亮 《铀矿地质》2010,26(2):73-79

文章应用活化构造成矿理论,对哈萨克斯坦古河道砂岩型S铀矿床进行成矿特征分析,并与层间氧化带砂岩型Ⅰ矿床的成矿特征进行对比,认为S铀矿床成矿受大地构造、古潜水成矿作用、层位和岩性岩相、断裂构造及岩浆岩等控制,铀成矿具有多阶段复成因的特点。据此,从对企业生产的角度提出一些建议。  相似文献   

Possible impact event in the Late Cambrian     

O.A. Korchagin  S.V. Dubinina  V.A. Tsel'movich  I.I. Pospelov 《世界地质(英文版)》2007,10(1)

  相似文献   

Major and Trace Element Characteristics of Apatites in Granitoids from Central Kazakhstan: Implications for Petrogenesis and Mineralization   总被引：1，自引：0，他引：1  

Mingjian CAO  Guangming LI  Kezhang QIN  Eleonora Yusupovha SEITMURATOVA  Yongsheng LIU 《Resource Geology》2012,62(1):63-83

This paper presents abundances of major and trace elements of apatites in granitic rocks associated with different types of ore deposits in Central Kazakhstan on the basis of electron probe microanalysis and laser ablation inductively coupled plasma mass spectrometry. Our results demonstrate that the concentrations and ratios of elements in apatites from different granitoid rocks show distinct features, and are sensitive to magma evolution, petrogenetic and metallogenetic processes. Apatites in the rocks associated with Mo‐W deposits have high content of F and MnO, low content of Cl, which may be indicative of sedimentary sources, while apatites from a Pb‐Zn deposit show relatively high content of Cl and low F content, which possibly suggest a high water content. In these apatites, Sr contents decrease, while Mn and Y contents increase with magma evolution. This relationship reflects that these elements in apatites are related with the degree of magmatic differentiation. Four types of REE patterns in apatites are identified. Type 1 character of highest (La/Yb)_N in apatites of Aktogai porphyry Cu‐Mo deposit, Sayak‐I skarn Cu deposit and Akzhal skarn Pb‐Zn depposit is likely produced by the crystallization of heavy REE‐enriched minerals. Type 2 character of upward‐convex light REE in apatite of Aktogai porphyries likely results from La‐enriched mineral crystallization. Type 3 feature of Nd depletion in apatites of East Kounrad and Zhanet deposits both from Mo‐W deposits primarily inherits the character of host‐rock. Type 4 apatites of Aktogai deposit and Akshatau W‐Mo deposit with wide range of REE contents may suggest that apatites crystallize under a wide temperature range. Three types of apatite with distinct redox states are identified based on Eu anomaly. The Aktogai apatite with slight negative Eu anomaly displays the most oxidized state of the magma, and the apatites of other samples at Aktogai, East Kounrad and Akzhal with moderate negative Eu anomaly show moderate oxidizing condition of these rocks, while the remaining apatites with strong En anomaly indicate a moderate reductive state of these rocks.  相似文献   

DEMOGRAPHIC POLARIZATION OF HOUSING AFFORDABILITY IN SIX MAJOR UNITED STATES METROPOLITAN AREAS     

《Urban geography》2013,34(4):296-323

This paper describes and analyses the geography and structure of the neighborhood residential preferences and residential satisfaction of the inhabitants of the medium-sized, post-Soviet city of Ust'-Kamenogorsk, Kazakhstan (population ca. 300,000). It is based on a questionnaire survey (N = 1516 + 320) conducted by the author in cooperation with the statistical authority of the Eastern Kazakhstan oblast'. At the aggregate level, the evidence that is presented suggests distinct preference patterns, and that the main focus of preference is on the city center. The geography of residential satisfaction is different. Differences in satisfaction have been found between residents of housing built by former high-priority enterprises and those occupying most of the remainder of the housing stock. These differences underscore the pervasive and continuing importance of the legacy of Soviet economic and territorial planning, and the still rather limited changes that the marketization of the economy has been able to produce.  相似文献   

The Circle of Hydro-Hegemony between riparian states,development policies and borderlands: Evidence from the Talas waterscape (Kyrgyzstan-Kazakhstan)     

《Geoforum》2017

Since the 1990s, transboundary water management has come to play a key role both in global environmental politics debates and in the shaping of international development policies, specifically in the Global South. As a consequence, a growing body of literature in the framework of critical hydropolitics has emerged reflecting on the role that power, discourses, and strategies play in shaping transboundary water policies and in influencing riparian relations. The focus on a state-centric perspective, however, often has led to neglect of the role of international development actors in shaping these policies. Through a critical application of the Circle of Hydro-Hegemony (CHH) and ethnographic qualitative field research in borderlands, this contribution aims to analyse how the establishment of a development initiative known as the Chu-Talas Commission, supported by the United Nations Economic Commission for Europe (UNECE) and other donors, has influenced and shaped transboundary water politics in the Talas waterscape, which is shared by Kyrgyzstan and Kazakhstan. The evidence shows that despite the international narration of the Chu-Talas Commission as a success story for water cooperation in Central Asia, Kazakhstan, through the deployment of both material and bargaining power strategies, has been able to shape UNECE development policies in its favour, impose its agenda on Kyrgyzstan, and emerge as the basin hydro-hegemon.  相似文献   

中亚成矿域核心区地质演化和巨型成矿带划分   总被引：10，自引：2，他引：8  

朱永峰 《矿床地质》2014,33(3):471-485

随着中亚成矿域地质矿产研究的不断升温和新资料的不断积累,学术界对其地质演化和成矿作用的认识出现诸多争议和矛盾。文章主要基于前苏联时期有关中亚地区的地质资料,并结合近年来地质矿产勘查新进展和高精度年代学数据,梳理了中亚成矿域核心区的主要地质特征及其演化规律,划分出中亚成矿域核心区的成矿省和巨型成矿带,论述了重要成矿带的形成和演化特征,并进行对比分析。在中亚成矿域核心区划分出4个成矿省：阿尔泰成矿省、巴尔喀什-准噶尔成矿省、楚伊犁-天山成矿省和西南天山成矿省,并重点论述了巴尔喀什-准噶尔成矿省和楚伊犁-天山成矿省的地质特征以及其中的巨型成矿带。巴尔喀什-准噶尔成矿省由4个巨型成矿带（含11个大型矿集区）组成：扎尔玛-萨吾尔成矿带、塔尔巴哈台-谢米斯台成矿带、阿科斗卡-巴尔鲁克成矿带和巴尔喀什-西准噶尔成矿带。楚伊犁-天山成矿省由4个巨型成矿带（含22个大型矿集区）构成：莫因特-阿拉套-赛里木成矿带、楚伊犁-博洛霍勒成矿带、伊赛克-阿吾拉勒成矿带和卡扎尔曼-那拉提成矿带。文中所提出的成矿省和巨型成矿带划分方案依然是初步的,在以后的工作中还需要不断修订和完善。我们期待着发现更多大型矿床和矿集区,使中亚成矿域核心区更丰富、更完善。地质资料的不断积累和新数据的不断补充,必然带动科学认识的提高和深化。  相似文献   

哈萨克斯坦斑岩铜矿地质-成因模式   总被引：1，自引：0，他引：1  

宋志齐  高鹏  祁世军  成守德 《新疆地质》2009,27(Z1)

简述了哈萨克斯坦斑岩铜矿的成矿特征并划分出3种类型,分别为次生石英岩化-泥化斑岩铜矿--科翁腊德(коунрадский)型;黄铁细晶岩化-粘土化斑岩铜矿--阿尔马林(алмалинсий)型;青磐岩化细脉浸染型斑岩铜矿--博萨库里(бозшакольский)型.其中,科翁腊德型最靠近地表,阿尔马林型居中,博萨库里型最深.对各类型铜矿的基本特征进行了概述.  相似文献   

Review of Cretaceous sauropod dinosaurs from Central Asia     

《Cretaceous Research》2017

There are 24 known localities for skeletal remains of sauropod dinosaurs in the republics of Central Asia (Kazakhstan, Kyrgyzstan, Tajikistan, and Uzbekistan). Sauropod remains are very rare at all these localities and represented usually only by isolated teeth. Only narrow-crowned teeth are known from the Cretaceous of Central Asia. The oldest record of such teeth is from the Aptian Sultanbobo Formation of Uzbekistan. Exposures of the Turonian Bissekty Formation at the most productive vertebrate locality in the region, Dzharakuduk in Uzbekistan, has yielded many isolated teeth and a few skeletal remains that can be attributed to a non-lithostrotian titanosaur. Similar narrow-crowned, cylindrical teeth from Cenomanian-to Coniacian-age strata in the Kyzylkum Desert, Uzbekistan, may belong to a closely related taxon. Another taxon, with teeth that are pentagonal in cross-section, is known from the Santonian Yalovach and Bostobe formations of Tajikistan and western Kazakhstan, respectively. A femur reported from the Santonian Syuksyuk Formation of southern Kazakhstan possibly belongs to a lithostrotian titanosaur. The change in tooth structure at the Coniacian–Santonian boundary in the region possibly suggests replacement of non-lithostrotian titanosaurs by lithostrotians. The titanosaur from the Bissekty Formation is similar to Dongyangosaurus sinensis from the Cenomanian–Turonian of Zhejiang (China) in the extensive pneumatization of the neural arch on the anterior caudal vertebrae with several fossae. It also resembles Baotianmansaurus henanensis from the Cenomanian of Henan (China) in the possession of very short anterior caudal centra. These three taxa possibly represent an as yet formally unrecognized endemic clade of Asian non-lithostrotian titanosaurs.  相似文献