A first Holocene leaf wax isotope-based paleoclimate record from the semi-humid to semi-arid south-eastern Caucasian lowlands     

Marcel Bliedtner  Roland Zech  Jana Zech  Imke Schäfer  Hans von Suchodoletz 《第四纪科学杂志》2020,35(5):625-633

The Holocene paleoclimate of the Caucasus region is rather complex and not yet well understood: while existing studies are mainly based on pollen records from high-altitude and humid lowland regions, no records are available from the semi-humid to semi-arid south-eastern Caucasian lowlands. Therefore, this study investigated compound-specific δ²H and δ¹³C isotopes of leaf wax biomarkers from Holocene floodplain soils in eastern Georgia. Our results show that the leaf wax δ²H signal from the paleosols mostly reflects changes in the moisture source and its isotopic composition. Depleted δ²H values before ~8 cal ka bp change towards enriched values after ~5 cal ka bp and become again depleted after ~1.6 cal ka bp. This trend could be caused by Holocene changes of the isotopic compositions of the Black and eastern Mediterranean Sea, and/or by varying contribution of both moisture sources linked with the North Atlantic Oscillation. The leaf wax δ¹³C signal from the paleosols directly indicates varying local water availability and drought stress. Depleted δ¹³C values before ~8 and after ~5 cal ka bp indicate wetter local conditions with higher water availability, whereas more enriched values during the middle Holocene (~8 until at least 5 cal ka bp ) indicate drier conditions with increased drought stress.  相似文献   

盈江县超上地区橄榄辉石岩脉地球化学特征、岩石成因及其构造环境     

赵宇新  方乙 《四川地质学报》2020,40(1):158-164

盈江县超上地区橄榄辉石岩脉的全岩地球化学特征表明:岩脉具有高Al、低Ti、贫P2O5和低碱的特点,属于低钾拉斑系列。另外具有与橄榄岩平衡的原生岩浆相一致的Mg#值为(70.89~72.18)、略微的Eu正异常(δEu=1.16~1.40),轻稀土元素富集,重稀土元素相对平缓;微量元素蛛网图上岩脉富集大离子亲石元素U、Th、Pb等,强烈亏损高场强元素Nb、Ta、Hf、P、Ti等。通过综合分析,认为岩脉岩浆源区为被俯冲板片流体改造过的亏损地幔,由其形成的母岩浆在演化过程中遭受了不同程度的下地壳物质的同化混染作用和有限的结晶分异作用,并可能经历了辉石的堆晶作用。结合区域资料,认为盈江县超上橄榄辉石岩脉形成于岛弧环境,超上地区可能在侏罗纪时期经历了中特提斯洋的俯冲消减。  相似文献   

基于"一带一路"建设的环渤海地区港口优势评价          下载免费PDF全文

赵江南  周跃 《海洋开发与管理》2019,36(7):83-88

港口作为海陆运输的节点,是一个城市和国家的重要门户,对推动经济发展和对外贸易有着不可忽视的作用。基于国家提出的"一带一路"建设,评估环渤海港口的发展优势,逐步实现从沿海、沿江开放向内陆延伸具有重要意义。文章选取环渤海港口中的大连、天津、唐山、丹东、营口、锦州、秦皇岛、黄骅、日照、青岛、威海和烟台共12个港口进行发展优势对比。从港口吞吐量、港口规模范围、港口城市及腹地、港口未来发展4个方面构建环渤海港口优势评价体系。并利用熵权-TOPSIS法进行深入的实证分析。结果表明,环渤海港口群港口发展优势水平悬殊,基本可以分为4个档次。基于此,环渤海各港口应合理准确定位,通过错位发展和协同合作等方式谋求共赢。  相似文献   

环渤海区域及邻区现今地壳构造运动形变特征分析     

赵旭坤  张俊  雷前坤  范成成 《大地测量与地球动力学》2019,39(11):1101-1105

将环渤海区域划分为5个次级块体，利用整体旋转与线性应变模型分析2009~2014年中国大陆构造环境监测网络的GPS对地观测速度场数据，得到相对于欧亚板块0.5°×0.5°的水平运动速度场和应变场。分析形变速度场和应变场的空间变化发现，环渤海区域整体上呈现0.25×10^-9/a的NW-SE 111.3°的双向趋势性扩张运动，太行块体、山西块体分别呈NW-SE 116.3°、NW-SE 130°的微弱扩张运动，胶辽块体、冀鲁块体和阴山-燕山块体分别存在NW-SE 144.3°、NE-SW 39.5°和NW-SE 155.6°的微弱压缩运动，其中太行块体的扩张运动量级相对于其他次级块体较大。尽管环渤海区域内部各次级块体的形变在空间上存在以上差异，但整体上环渤海区域主压应变轴方向基本为NEE-SWW，主张应变轴方向为NNW-SSE，且主压应变轴走向为NE 47.70°～89.74°，与利用地球物理方法得到的主压应变轴优势方向大体一致，表明环渤海区域现今地壳运动相对稳定。  相似文献   

Watershed delineation using hydrographic features and a DEM in plain river network region          下载免费PDF全文

Zhengqing Lai  Shuo Li  Guonian Lv  Zhirong Pan  Guosong Fei 《水文研究》2016,30(2):276-288

Watershed delineation is a required step when conducting any spatially distributed hydrological modelling. Automated approaches are often proposed to delineate a watershed based on a river network extracted from the digital elevation model (DEM) using the deterministic eight‐neighbour (D8) method. However, a realistic river network cannot be derived from conventional DEM processing methods for a large flat area with a complex network of rivers, lakes, reservoirs, and polders, referred to as a plain river network region (PRNR). In this study, a new approach, which uses both hydrographic features and DEM, has been developed to address the problems of watershed delineation in PRNR. It extracts the river nodes and determines the flow directions of the river network based on a vector‐based hydrographic feature data model. The river network, lakes, reservoirs, and polders are then used to modify the flow directions of grid cells determined by D8 approach. The watershed is eventually delineated into four types of catchments including lakes, reservoirs, polders, and overland catchments based on the flow direction matrix and the location of river nodes. Multiple flow directions of grid cells are represented using a multi‐direction encoding method, and multiple outflows of catchments are also reflected in the topology of catchments. The proposed approach is applied to the western Taihu watershed in China. Comparisons between the results obtained from the D8 approach, the ‘stream burning’ approach, and those from the proposed approach clearly demonstrate an improvement of the new approach over the conventional approaches. This approach will benefit the development of distributed hydrological models in PRNR for the consideration of different types and multiple inlets and outlets of catchments. Copyright © 2015 John Wiley & Sons, Ltd.  相似文献   

A late Quaternary vertebrate deposit in Kudjal Yolgah Cave,south‐western Australia: refining regional late Pleistocene extinctions          下载免费PDF全文

Nathan R. Jankowski  Grant A. Gully  Zenobia Jacobs  Richard G. Roberts  Gavin J. Prideaux 《第四纪科学杂志》2016,31(5):538-550

  相似文献   

新疆北山地区罗东镁铁质-超镁铁质层状岩体岩石成因   总被引：4，自引：0，他引：4  

凌锦兰  夏明哲  郭娜欣  汪帮耀  夏昭德  姜常义 《地球化学》2011,(6):499-515

罗东镁铁质-超镁铁质岩体位于塔里木板块东北部的新疆北山地区,岩体平面形态为眼球状,出露面积约2.1 km2.由纯橄岩、单辉橄榄岩、斜长二辉橄榄岩、橄榄二辉岩、方辉辉石岩、橄长岩、橄榄辉长岩、辉长岩、苏长辉长岩和淡色辉长岩组成,堆晶结构和堆晶韵律发育,属于层状岩体.岩浆演化过程中主要分离结晶/堆晶相是橄榄石和单斜辉石,此...  相似文献   

CSAMT与SIP物探组合法在河南省栾川山区隐伏金属矿勘查中的应用   总被引：2，自引：0，他引：2  

马振波 《地质与勘探》2011,47(4):654-662

目前隐伏金属矿产勘查的深度逐渐加大,勘查区也逐渐向工作程度相对较低、情况更加复杂的山区转移,常规的、单一的物探方法在勘探深度及精度等方面都已经无法满足目前勘查的需要。针对这种情况,本文提出可控源音频大地电磁测深法（CSAMT）与频谱激电法（SIP）的技术组合,并将其运用于河南栾川山区隐伏金属矿勘查实践中。结果表明该方法...  相似文献   

下扬子地区中-新生代的挤压变形与伸展改造及其油气勘探意义   总被引：7，自引：3，他引：4  

李海滨  贾东  武龙  张勇 《岩石学报》2011,27(3):770-778

以地表变形特征、地层厚度变化和地震剖面为约束,构建了贯穿下扬子地区主要构造单元的三条地质大剖面。剖面展示了研究区早期褶皱逆冲、晚期伸展断陷的构造格局,并揭示了变形的空间差异。通过对褶皱卷入的层位、断层与地层的切割关系及不整合类型和发育特征的梳理,得出研究区北侧的褶皱逆冲主要形成于中-晚三叠世,南侧的褶皱逆冲主要形成 于中-晚侏罗世。两侧的挤压构造在晚白垩世开始都经历了强烈的拉张作用,北侧的断陷一直持续到古近纪,新近纪以拗陷为主,而南侧古近纪断陷规模较小,新近纪拗陷不发育。苏州-无锡地区的下古生界受后期改造作用较弱,是油气勘探的有利地区。  相似文献   

诸广山南部白云岩体岩石地球化学特征及成因     

张善果  黄国龙  沈渭洲  伏顺成  王小冬  许丽丽 《铀矿地质》2011,(5):265-273,281

白云岩体位于诸广山南部岩体中东部,是一个重要的产铀岩体,其岩性为粗粒斑状黑云母花岗岩。在主量元素方面,该岩体的岩石富硅（SiO2平均为73.47%）、富铝（A/CNK值平均为1.09）和高的K2O/Na2O值（平均为1.99）;在微量元素方面,富集大离子元素Rb、Th,而Ba、Sr、Ti、Nb、Ta、P亏损明显,具有高的Rb/Sr（平均为6.22）和Rb/Nb值（平均为29.07）,富含铀（平均为9.04×10-6）,可为岩体内铀矿床的形成提供铀源;轻稀土元素富集和轻、重稀土元素分馏相对明显,稀土元素配分曲线呈右倾型,Eu亏损明显;在同位素方面,εNd（t）值低（平均为-10.6）,（87Sr/86Sr）i值高（平均为0.71688）,Nd模式年龄古老（1865～1874 Ma）。这些特征表明,白云岩体属于典型的壳源型花岗岩,是在华南地块和印支地块碰撞结束后不久形成的伸展构造环境中,位于地壳中-下部的古-中元古代地壳组分在伸展、减薄作用产生的减压、导水和地幔上涌等因素的综合影响下,由泥质岩源区发生部分熔融而形成。  相似文献