Intercalibration of age readings of ling (Molva molva L.) blue ling (Molva dipterygia Pennant, 1784) and tusk (Brosme brosme L.)     

Bergstad  O. A.; Magnusson  J. V.; Magnusson  J.; Hareide  N. -R.; Reinert  J. 《ICES Journal of Marine Science》1998,55(2):309-318

  相似文献   

浑善达克沙地的形成时代与成因初步研究   总被引：30，自引：8，他引：22  

李孝泽  董光荣 《中国沙漠》1998,18(1):16-21

根据较广泛的含风成砂地层的野外调查与有关室内样品分析结果,浑善达克沙地至少形成于晚第三纪。当时受暖干亚热带动力高压控制和较弱东亚季风影响,出现温暖干旱荒漠、半干旱草原及森林草原之间的环境变化,形成亚热带红色季风性沙漠沉积。第四纪,受东亚季风及其变迁影响,环境在温带荒漠草原至森林草原之间波动变化,出现一系列沙丘活化、沙漠扩展与沙丘固定、沙漠收缩的波动过程,形成温带黄色季风型沙漠沉积。  相似文献   

黄土高原末次间冰期气候的不稳定性特征   总被引：3，自引：0，他引：3  

李铮华  叶浩  陈云  王玉海  张俊牌 《地质力学学报》1998,4(4):46-49,75

欧共体格陵兰冰芯计划(GRIP)中的冰芯资料揭示末次间冰期气候具有快速变化的不稳定性特征,而美国格陵兰冰盖计划(GISP2)却不曾发现其不稳定证据。本文通过黄土高原诸剖面的古气候代用指标综合分析认为,末次间冰期,特别是早期气候曾出现过较大幅度的气候波动,存在不稳定性特征,支持了GRIP结果,表明中国黄土含有极地北大西洋的气候信息,是全球变化研究的理想记录。   相似文献   

基于贝壳生长轮方法的平端深海偏顶蛤的生长和年龄结构研究          下载免费PDF全文

胡希源  周丽  李超伦 《海洋与湖沼》2023,54(2):465-471

平端深海偏顶蛤(Gigantidasplatifrons)是广泛分布于西太平洋深海热液和冷泉生态系统中的优势种和共有种,也是深海化能生态系统中重要的生境营造种。以南海F冷泉平端深海偏顶蛤为研究对象,基于贝壳日生长轮方法,分析了平端深海偏顶蛤的年龄与生长速率,建立了其年龄与贝壳壳长关系的生长方程。同时,结合获得的生长方程,分析了南海F冷泉采样点(119.285 6°E,22.115 4°N)平端深海偏顶蛤种群的年龄结构。研究结果表明,采样获得的平端深海偏顶蛤种群的最大壳长为11.4 cm,最大寿命为13.5龄。研究区域的贝壳长度分布集中在4～7 cm,占比60%;年龄分布集中在2～4龄,占比49.7%。相关研究结果为进一步开展平端深海偏顶蛤的生长研究提供了基础数据,有助于深入了解冷泉区域的种群动态变化规律。  相似文献   

Late Eocene–early Miocene provenance evolution of the Crocker Fan in the southern South China Sea     

Yuchi Cui  Lei Shao  Wu Tang  Peijun Qiao  Goh Thian Lai  Yongjian Yao 《海洋学报(英文版)》2023,42(3):215-226

There are many large-scale Cenozoic sedimentary basins with plentiful river deltas, deep-water fans and carbonate platforms in the southern South China Sea. The Crocker Fan was deposited as a typical submarine fan during the late Eocene–early Miocene, and stretches extensively across the entire Sarawak–Sabah of the northern Borneo area. However, systematic analyses are still lacking regarding its sediment composition and potential source suppliers. No consensus has been reached yet on the provenance evolution and sedimentary infilling processes, which seriously impeded the oil-and-gas exploration undertakings. By combining with sedimentary-facies identification, heavy mineral assemblages, elemental geochemistry and detrital zircon U-Pb dating, this paper aims to generalize an integrated analysis on the potential provenance terranes and restore source-to-sink pathways of the Crocker Fan. In general, the Crocker Fan was initially formed over the Cretaceous–lower/middle Eocene Rajang Group by an angular Rajang unconformity. The continual southward subduction of the proto-South China Sea resulted in magmatic activities and subsequent regional deformation and thrusting along the Lupar Line in the northern Borneo. The lowermost Crocker sequence is featured by a thick conglomerate layer sourced from in-situ or adjacent paleo-uplifts. From the late Eocene to the early Miocene, the Crocker Fan was constantly delivered with voluminous detritus from the Malay Peninsula of the western Sundaland. The Zengmu Basin was widely deposited with delta plain and neritic facies sediments, while the Brunei-Sabah Basin, to the farther east, was ubiquitously characterized by turbiditic sequences. The Crocker Fan successions are overall thick layers of modest-grained sandstones, which formed high-quality reservoirs in the southern South China Sea region.  相似文献   

吉林红旗岭铜镍硫化物矿床的成矿时代讨论   总被引：14，自引：2，他引：12  

郗爱华  顾连兴  李绪俊  叶松青  郑远川 《矿床地质》2005,24(5):521-526

通过对红旗岭铜镍硫化物矿床1号含矿超镁铁质岩体和8号不含矿镁铁-超镁铁质岩体进行单矿物40Ar-39Ar法测年,得到与铜镍硫化物矿床相关的角闪石与黑云母结晶年龄分别为250 Ma和225 Ma,这一结果与前人所报道的K-Ar法年龄有明显的差异.结合与热液矿化相关的斜长伟晶岩锆石SHRIMP法年龄216 Ma,认为镁铁-超镁铁质岩形成于250 Ma左右的印支早期,铜镍硫化物矿床的形成时间晚于含矿岩体,大约为225 Ma前后的印支中期.216 Ma前后的岩浆期后热液叠加对成矿具有积极作用.  相似文献   

滇西腾冲大硐厂铜-铅-锌矿床的辉钼矿Re-Os同位素定年   总被引：5，自引：1，他引：4  

董方浏  侯增谦  高永丰  曾普胜  蒋成兴  杜安道 《矿床地质》2005,24(6):663-668

在环绕印度—亚洲大陆碰撞形成的东构造结波密—腾冲弧形构造带中,发育一组含锡铅_锌_铜多金属矿床,但一直没有准确的成矿年龄数据。文章通过对大硐厂铅_锌矿区红沟岩铜矿体中辉钼矿的Re_Os同位素测试,获得精确的成矿等时线年龄为(118.0±2.4)Ma。区内与成矿关系密切的斑岩成岩年龄在143～112Ma,认为斑岩成岩与成矿同期,同为燕山晚期。  相似文献   

Tephra isochrons and chronologies of colonisation     

《Quaternary Geochronology》2017

This paper demonstrates the use of tephrochronology in dating the earliest archaeological evidence for the settlement of Iceland. This island was one of the last places on Earth settled by people and there are conflicting ideas about the pace and scale of initial colonisation. Three tephra layers, the Landnám (‘land-taking’) tephra layer (A.D. 877 ± 1), the Eldgjá tephra (A.D. 939) and the recently dated V-Sv tephra (A.D. 938 ± 6) can be found at 58% of 253 securely-dated early settlement sites across the country. The presence of the tephras permits both a countrywide comparison, and a classification of these settlement sites into pre-Landnám, Landnám and post-Landnám. The data summarised here for the first time indicate that it will be possible to reconstruct the tempo and development of the colonisation process in decadal resolution by more systematically utilising the dating potential of tephrochronology.  相似文献   

西太平洋海山区构造分区图编制及玄武岩Nd同位素填图     

王历星  姚会强  李正刚  刘丽强  韩冰  彭天玥 《海洋地质与第四纪地质》2021,41(1):180-191

基于公开的地球物理、地球化学数据以及国内外航次调查积累的海底地形等资料,笔者编制了西太平洋海山区1∶500万构造分区图。西太平洋海山区构造分区图包括1幅主图和3幅辅图,主图为《西太平洋海山区构造分区图》,共划分出了3个一级板块、22个二级分区块体、12个三级分区块体,3幅辅图分别为《西太平洋海山区地质构造图》、《西太平洋海山区布格重力异常图》和《西太平洋海山区εNd(t)等值线图》。本文介绍了构造分区图编制的思路和方法、数据来源和构造单元的划分依据,还通过搜集和整理西太平洋海山区玄武岩εNd(t)同位素数据,在研究区圈定了9个Nd同位素异常区,并讨论了Nd同位素填图结果与地质过程的耦合关系以及其对海山区构造分区的指示意义。  相似文献   

Continuous real‐time analysis of the isotopic composition of precipitation during tropical rain events: Insights into tropical convection          下载免费PDF全文

Shaoneng He  Nathalie F. Goodkin  Dominik Jackisch  Maria Rosabelle Ong  Dhrubajyoti Samanta 《水文研究》2018,32(11):1531-1545

To investigate stable isotopic variability of precipitation in Singapore, we continuously analysed the δ‐value of individual rain events from November 2014 to August 2017 using an online system composed of a diffusion sampler coupled to Cavity Ring‐Down Spectrometer. Over this period, the average value (δ¹⁸O_Avg), the lowest value (δ¹⁸O_Low), and the initial value (δ¹⁸O_Init) varied significantly, ranging from ?0.45 to ?15.54‰, ?0.9 to ?17.65‰, and 0 to ?13.13‰, respectively. All 3 values share similar variability, and events with low δ¹⁸O_Low and δ¹⁸O_Avg values have low δ¹⁸O_Init value. Individual events have limited intraevent variability in δ‐value (Δδ) with the majority having a Δδ below 4‰. Correlation of δ¹⁸O_Low and δ¹⁸O_Avg with δ¹⁸O_Init is much higher than that with Δδ, suggesting that convective activities prior to events have more control over δ‐value than on‐site convective activities. The d‐excess of events also varies considerably in response to the seasonal variation in moisture sources. A 2‐month running mean analysis of δ¹⁸O reveals clear seasonal and interannual variability. Seasonal variability is associated with the meridional movement of the Intertropical Convergence Zone and evolution of the Asian monsoon. El Niño–Southern Oscillation is a likely driver of interannual variability. During 2015–2016, the strongest El Niño year in recorded history, the majority of events have a δ¹⁸O value higher than the weighted average δ¹⁸O of daily precipitation. δ¹⁸O shows a positive correlation with outgoing longwave radiation in the western Pacific and the Asian monsoon region, and also with Oceanic Niño Index. During El Niño, the convection centre shifts eastward to the central/eastern Pacific, weakening convective activities in Southeast Asia. Our study shows that precipitation δ‐value contains information about El Niño–Southern Oscillation and the Intertropical Convergence Zone, which has a significant implication for the interpretation of water isotope data and understanding of hydrological processes in tropical regions.  相似文献