新疆博州地区近46年来的气候变化特征   总被引：23，自引：4，他引：23  

辛渝  张广兴  张新  博力健 《干旱区地理》2006,29(2):193-200

根据新疆博尔塔拉蒙古自治州(简称博州,下同)四个气象代表站点的气温及降水资料,利用线性趋势函数及t检验法分析了该地区近46年的气候变化。结果表明,博州年平均气温、平均最高气温、平均最低气温均呈上升趋势,而且平均最低气温上升的幅度远大于平均最高气温的上升幅度。年平均气温及年平均最低气温约在20世纪80年代中期出现了显著的均值突变,而年平均最高气温在80年代末出现突变;除春、夏季平均最高气温无明显变化趋势外,其它各季平均气温、平均最高气温、平均最低气温均呈上升趋势,其中均以冬季增幅最大,秋季次之;80年代冬夜升温最强劲,90年代则明显减弱;夏季的平均气温与平均最低气温均在70年代中期出现突变,比其它任何突变时间都早;暖温年多发生在80年代后,冷温年多发生在20世纪60年代、70年代。年降水量略呈上升趋势,少雨年多在60年代、70年代,多雨年多在近20年,除春季外,其余各季降水略有上升趋势。  相似文献   

Middle Paleozoic paleomagnetism of east Kazakhstan: post-Middle Devonian rotations in a large-scale orocline in the central Ural–Mongol belt     

Natalia M. Levashova  Kirill E. Degtyarev  Mikhail L. Bazhenov  Adam Q. Collins  Rob Van der Voo   《Tectonophysics》2003,377(3-4):249-268

In order to test different hypotheses concerning the Paleozoic evolution of the Ural–Mongol belt (UMB) and the amalgamation of Eurasia, we studied Middle Devonian basalts from two localities (11 sites) and Lower Silurian volcanics, redbeds, and intra-formational conglomerates from three localities (20 sites) in the Chingiz Range of East Kazakhstan. The Devonian rocks prove to be heavily overprinted in the late Paleozoic, and a high-temperature, presumably primary, southerly, and down component is isolated at only four sites from a homoclinal section. Most Silurian redbeds are found to be remagnetized in the late Paleozoic; in contrast, a bipolar near-horizontal remanence, isolated from Silurian volcanics, is most probably primary as indicated by positive tilt and conglomerate tests. Analysis of paleomagnetic data from the Chingiz Range shows that southward-pointing directions in Ordovician, Silurian, and Devonian rocks are of normal polarity and hence indicate large-scale rotations after the Middle Devonian. The Chingiz paleomagnetic directions can be compared with Paleozoic data from the North Tien Shan and with the horseshoe-shaped distribution of subduction-related volcanic complexes in Kazakhstan. Both paleomagnetic and geological data support the idea that today's strongly curved volcanic belts of Kazakhstan are an orocline, deformed mostly before mid-Permian time. Despite the determination of nearly a dozen new Paleozoic paleopoles in this study and other recent publications by our team, significant temporal and spatial gaps remain in our knowledge of the paleomagnetic directions during the middle and late Paleozoic. However, the paleomagnetic results from the Chingiz Range and the North Tien Shan indicate that these areas show generally coherent motions with Siberia and Baltica, respectively.  相似文献   

Middle Jurassic–Early Cretaceous tectonic evolution of the Bayanhushuo area,southern Great Xing’an Range,NE China: constraints from zircon U–Pb geochronological and geochemical data of volcanic and subvolcanic rocks     

Qing-Bin Guan  Bin Wang  Xiong Wang  Xing-An Wang  Qiang Shi 《International Geology Review》2018,60(15):1883-1905

This study presents new zircon U–Pb geochronology, geochemistry, and zircon Hf isotopic data of volcanic and subvolcanic rocks that crop out in the Bayanhushuo area of the southern Great Xing’an Range (GXR) of NE China. These data provide insights into the tectonic evolution of this area during the late Mesozoic and constrain the evolution of the Mongol–Okhotsk Ocean. Combining these new ages with previously published data suggests that the late Mesozoic volcanism occurred in two distinct episodes: Early–Middle Jurassic (176–173 Ma) and Late Jurassic–Early Cretaceous (151–138 Ma). The Early–Middle Jurassic dacite porphyry belongs to high-K calc-alkaline series, showing the features of I-type igneous rock. This unit has zircon ε_Hf(t) values from +4.06 to +11.62 that yield two-stage model ages (T_DM2) from 959 to 481 Ma. The geochemistry of the dacite porphyry is indicative of formation in a volcanic arc tectonic setting, and it is derived from a primary magma generated by the partial melting of juvenile mafic crustal material. The Late Jurassic–Early Cretaceous volcanic rocks belong to high-K calc-alkaline or shoshonite series and have A₂-type affinities. These volcanics have ε_Hf(t) and T_DM2 values from +5.00 to +8.93 and from 879 to 627 Ma, respectively. The geochemistry of these Late Jurassic–Early Cretaceous volcanic rocks is indicative of formation in a post-collisional extensional environment, and they formed from primary magmas generated by the partial melting of juvenile mafic lower crust. The discovery of late Mesozoic volcanic and subvolcanic rocks within the southern GXR indicates that this region was in volcanic arc and extensional tectonic settings during the Early–Middle Jurassic and the Late Jurassic–Early Cretaceous, respectively. This indicates that the Mongol–Okhotsk oceanic plate was undergoing subduction during the Early–Middle Jurassic, and this ocean adjacent to the GXR may have closed by the Late Middle Jurassic–Early Late Jurassic.  相似文献   

内蒙中部玄武岩残坡积膨胀土的研究     

王玉洲  曲永新 《工程地质学报》1995,3(2):12-20

本文是我们在内蒙中部所发现的一种新型膨胀土即玄武岩残积粘土的宏观微观综合研究结果。本文揭示了在内蒙中部异常发育的残积粘土的特殊的形成环境，并从物质成分、物理化学性质、微结构等方面探讨了不良工程特性形成的机理，并进行了膨胀土的工程评价。这类膨胀土在我国北方的发现，改变了对我国北方膨胀土形成发育规律的认识。  相似文献   

白云鄂博碳酸岩墙碳氧同位素地球化学   总被引：7，自引：3，他引：7  

舒勇  郑永飞  魏春生  周建波  杨学明  杨晓勇 《地球化学》2001,30(2):169-176

对内蒙古白云鄂博 REE- Fe- Nb矿床周围碳酸岩墙中共存的方解石和白云石进行了 C和 O同位素分析。结果表明，方解石和白云石的δ 13C值变化范围一致，均为－ 3.5‰～－ 7.3‰，落在正常地幔δ 13C值范围 (－ 5‰± 2‰ )内；而它们的δ 18O值可分为两组，第Ⅰ 组为 9.5‰～ 18.0‰，第Ⅱ 组为 20.6‰～ 22.6‰，均远大于正常地幔δ 18O值范围 (5.7‰± 1.0‰ )。第Ⅰ 组低δ 18O值样品中共存白云石与方解石之间的 C和 O同位素分馏均为负值，因此处于热力学不平衡状态，指示它们自形成后受到过后期热液蚀变，与先前的岩石学观察一致。相反，第Ⅱ 组高δ 18O值样品中白云石与方解石之间的 C和 O同位素分馏均为正值，处于热力学平衡状态，指示它们自形成后未受到后期热液蚀变，因此可能沉淀于晚期低温高δ 18O值流体。第Ⅰ 组碳酸岩墙中白云石的 C和 O同位素组成不呈线性分布，指示碳酸岩浆并非由幔源碳酸盐与沉积碳酸盐混合形成。应用水-岩交换模型计算得到，第Ⅰ 组碳酸岩在侵位后经历了碳酸岩浆期后热液的不均一蚀变，蚀变温度约在 220～ 800℃之间，蚀变流体的 CO2/H2O比值较小 (1/500)，但水 /岩比值变化较大 (10～ 400)。由于低温下方解石与热液之间的碳氧同位素交换速率大于白云石，导致这部分碳酸  相似文献   

甘蒙北山中南带新发现燕山早期走滑挤压推覆构造带   总被引：5，自引：0，他引：5       下载免费PDF全文

左国朝  郑亚东 《地质科学》1992,(4):309-316

近年来在区域调查基础上,于甘蒙北山中南带首次发现了六条由南向北推覆的构造带,在每个推覆陶造带边缘发育大小不一的飞来峰。推覆体走向近东西,推覆在震旦系至中、下侏罗统之上,最大直观推覆距达55km,累积推覆距大于150km,并被上侏罗统不整合覆盖,形成时代为燕山早期。  相似文献   

巴尔哲碱性花岗岩稀有稀土矿床地质特征及成因探讨     

冯守忠 《矿产与地质》1993,7(1):43-48

内蒙古巴尔哲碱性花岗岩稀有稀土特大型矿床是国内首次发现的一种新类型工业矿床,其规模居亚洲第三位.含矿岩体为燕山期碱性花岗岩,岩体普遍矿化,岩体即是矿体,矿石品位富,稀有稀土元素种类多,其共生伴生矿物多达44种,工业矿物以羟硅铍钇铈矿、烧绿石、铌铁矿、锌日光榴石为主.  相似文献   

能源基地晋陕蒙接壤地区地质环境质量定量研究     

何荣文 《陕西地质》1993,(2)

本文基于地质环境是由诸多因素有机组合而成,其质量也是各因素质量的复杂组合,是一种模糊现象,难以精确评价,但又存在明显差异的认识,采用模糊数学理论,即以环境地质亚区为单元,考虑多因素的综合影响。采用数量化的动态聚类法,对晋陕蒙接壤地区地质环境质量进行了评价:包括自然条件下地质环境质量评价和煤炭、水资源开发后地质环境质量的相对变化评价。  相似文献   

A New Titanosaurian Sauropod from Late Cretaceous of Nei Mongol, China   总被引：2，自引：0，他引：2  

XU Xing ZHANG Xiaohong TAN Qingwei ZHAO Xijin TAN Lin 《《地质学报》英文版》2006,80(1):20-26

A specimen collected from the Upper Cretaceous Erlian Formation of Nei Mongol （Inner Mongolia）, China, represents a new genus and species of titanosaurian sauropod. The new taxon is named and described on the basis of the holotype and the only known specimen, which comprises several dorsal, sacral, and caudal vertebrae, several dorsal ribs, one anterior chevron, and much of the pelvis. Diagnostic features of the new species include a thick ridge extending down from the postzygapophysis on the lateral surface of the neural arch of the posterior dorsal vertebrae, a transversely oriented accessory lamina present between the anterior centroparapophyseal limina and the lateral centraprezygapophyseal lamina of the posterior dorsal vertebrae, long, anteroventrally directed caudal rib that bears two distinctive fossae on its posterior margin on the anterior caudal vertebrae and a prominent vertical ridge above the pubic peduncle on the medial surface of the ilium, among others. The ilium is pneumatic, a feature not common among non-avian dinosaurs. The new taxon has an unusual combination of primitive and derived character states. Preliminary character analysis shows a complex character distribution within the Titanosauriformes. Recent titanosauriform discoveries suggest that a significant radiation occurred in Asia early in the titanosauriform evolution.  相似文献   

塔里木河中下游城镇化进程中水资源利用分析   总被引：3，自引：0，他引：3       下载免费PDF全文

王长建  张小雷  杜宏茹  李雪梅 《干旱区地理》2012,35(2):324-331

 基于2000-2008年的统计数据,通过比较和定量分析塔里木河中下游巴音郭楞蒙古自治州（以下简称巴州）各县市城镇化水平与用水总量、用水效益、产业结构和用水结构的变化过程,建立城镇化水平与用水效益、用水总量之间的数学关系。结果表明：巴州各市县的用水效益都在不断提高,基本上是城镇化水平越高的地方其用水效益也高。城镇化水平与用水效益呈线性增长关系,巴州整体城镇化水平的提升对用水效益的增加有较大影响,城镇化水平提升一个百分点,用水效益增加2.62 元/m3。巴州的城镇化水平与用水总量之间对数增长关系不明显,水资源对城市化进程存在明显的约束作用。今后需要促进产业结构优化升级,提升水资源开发利用水平,提高用水效益,促进城镇化发展与水资源开发利用呈现出城市化水平高、用水总量低、用水效益高的高水平协调状态。  相似文献