黑龙江嘉荫与俄罗斯远东Kundur地区黑龙江杂岩锆石U-Pb年代学、Hf同位素组成及其地质意义   总被引：1，自引：1，他引：0  

孙晨阳  龙欣雨  许文良  王枫  葛文春  郭鹏  刘小杨 《岩石学报》2018,34(10):2901-2916

本文报道了黑龙江嘉荫和俄罗斯远东Kundur(昆杜尔)地区黑龙江杂岩锆石U-Pb年代学和Hf同位素分析结果,并结合前人研究成果,探讨了黑龙江杂岩的物质组成、形成时代、构造就位时间及物源。黑龙江嘉荫地区黑龙江杂岩中两个石榴石白云母石英片岩(13HYC28-1和13HYC29-1)原岩为流纹岩,其锆石U-Pb年龄分别为185±1Ma和183±1Ma,应代表黑龙江杂岩中存在的中酸性火山岩原岩的形成时代;俄罗斯远东Kundur(昆杜尔)地区石榴石二云母片岩(14RF4-1)和白云母石英片岩(14RF5-1)碎屑锆石年龄频谱主要存在两个年龄区间:183～286Ma和420～525Ma,另外还有少量前寒武纪年龄。这些碎屑锆石年龄组合与佳木斯地块和松嫩-张广才岭地块东缘发育的岩浆事件相对应,揭示其沉积物源应来自于这些火成岩。黑龙江杂岩碎屑锆石年龄数据中早侏罗世的最小峰期年龄(188Ma)代表了黑龙江杂岩原岩成岩时代的下限,结合区内177～165Ma的单矿物变质变形年龄,可以判定黑龙江杂岩的构造就位时间为早侏罗世晚期-中侏罗世。黑龙江杂岩的形成与就位过程揭示了东北亚陆缘早中生代的构造演化历史:中-晚三叠世(240～230Ma),牡丹江洋沿嘉荫-牡丹江断裂裂开并逐渐扩张,早侏罗世期间,古太平洋板块开始向欧亚大陆之下俯冲,受其影响,牡丹江洋俯冲并闭合于早侏罗世晚期-中侏罗世,最终导致佳木斯地块与松嫩-张广才岭地块碰撞拼合以及黑龙江杂岩的构造就位。  相似文献   

Siliceous-volcanogenic complexes of western Sikhote Alin: Their stratigraphy and origin     

A. N. Filippov  I. V. Kemkin 《Russian Journal of Pacific Geology》2009,3(2):154-168

New age and structural data are reported for the siliceous-volcanogenic complexes developed in the lower reaches of the Ussuri River. These complexes, which were previously treated as one stratigraphic unit, are subdivided into the Snarsky tectonostratigraphic complex (end of the Middle Jurassic-Middle Aptian) and the basaltic sequence (supposedly, Campanian-Maastrichtian). The Snarsky Complex is made up of basic volcanics, cherts, siliceous-clayey rocks, as well as subordinate limestones, sandstones, and conglomerates. Its distinctive features are the large amounts of genetically diverse basalts, the abundance of volcanomictic and pyroclastic material in siliceous-clayey rocks, the absence of fragmental rocks typical of the continental convergent zone, and the facies heterogeneity of the deposits. The complex is considered to be the southwestern continuation of the Kiselevka-Manoma terrane. Its origin is presumably related to the tectonic piling of genetically heterogeneous assemblages. The basaltic sequence includes basalts, basaltic andesites, their tuffs, and tuff conglomerates. The tuff conglomerates contain numerous fragments of granites and garnet-bearing felsic volcanics. The sequence was formed on the crystalline paleocontinental basement in the Late Cretaceous.  相似文献   

Palynological evidence for dating Jurassic-Cretaceous boundary sediments in the Bureya basin, Russian Far East     

V. S. Markevich  E. V. Bugdaeva 《Russian Journal of Pacific Geology》2009,3(3):284-293

Palynological complexes from the coaliferous Talyndzhan and Dublikan formations of the Bureya sedimentary basin are analyzed. The palynological assemblage from the upper part of the Talyndzhan Formation is characterized by dominant gymnosperms largely close to Pinaceae and Ginkgocycadophytus. The content of ferns is insignificant against the background of their relatively high taxonomic diversity. The assemblage is marked by the last occurrence of Staplinisporites pocockii, Camptotriletes cerebriformis, C. nitida, and Cingulatisporites sanguinolentus spores typical of the Late Jurassic palynofloras. The palynological assemblage from the Dublikan Formation is dominated by Pteridophyts representing mainly by Cyathidites and Duplexisporites. In addition to the conifer, the role of Classopollis increased among the gymnosperms in this assemblage. It also includes the first-appearing Stereisporites bujargiensis, Neoraistrickia rotundiformis, Contignisporites dorsostriatus, Duplexisporites pseudotuberculatus, D. rotundatus, Appendicisporites tricostatus, and Concavissimisporites asper. These sporomorphs are characteristic of the Berriasian palynofloras. Thus, the Jurassic-Cretaceous boundary is most likely located between the Talyndzhan and Dublikan formations.  相似文献   

The postal-geographical location: the notion and measurement algorithm (exemplified by the postal network of Siberia in the early 20th century)     

V.I. Blanutsa 《Geography and Natural Resources》2010,31(4):308-316

An analysis is made of the problems, approaches and methods in the study of the economic-geographical location. The term “postalgeographical location” is suggested. The concept of the location of a settlement in the postal network is formulated. The algorithm has been developed for measuring the postal-geographical location. Results from assessing the location of settlements in Siberia's postal network are presented for the year 1910.  相似文献   

1990年代以来俄罗斯社会经济地理学的发展     

吴淼  杨兆萍  戴颂英 《世界地理研究》2009,18(1):157-164

回顾上世纪90年代以前俄罗斯社会经济地理学的发展历程,阶段性和二元性是这一时期的主要特征．且受意识形态影响较大。1990年代以来,受西方人文地理学的理论、学说和研究方法以及国际大环境的影响,社会经济发展的驱动,社会和人文因素逐渐被重视;自然地理与社会经济地理二元化的现状正逐渐转向一体化发展的道路;经济化、社会化、人文化和生态化是当前俄罗斯社会经济地理学发展的主要特征。与此同时,科学理论研究不足、实践性不强和微观领域研究不足等是当前存在的主要问题。  相似文献