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321.
May-June precipitation reconstruction of southwestern Anatolia, Turkey during the last 900 years from tree rings 总被引:1,自引:0,他引:1
A May-June precipitation reconstruction (AD 1097-2000) has been developed for southwestern Anatolia in Turkey, the longest reported to date in this region. The reconstruction was derived from a regional Juniperus excelsa chronology that was built from material sampled at four sites in the Antalya and Mersin Districts. The regional tree-ring chronology accounts for 51% of the variance of instrumentally observed May-June precipitation. The years AD 1518 to 1587 are the most humid period in the reconstruction, coinciding with a major shift in European climate. The driest 70-year period in the reconstruction is AD 1195 to 1264. The period AD 1591-1660 represents the third driest and was characterized by instability climatically, politically, and socially in Anatolia. 相似文献
322.
Lesleigh Anderson Mark B. Abbott Bruce P. Finney Stephen J. Burns 《Quaternary Research》2005,64(1):21-35
Analyses of sediment cores from Jellybean Lake, a small, evaporation-insensitive groundwater-fed lake, provide a record of changes in North Pacific atmospheric circulation for the last ∼7500 yr at 5- to 30-yr resolution. Isotope hydrology data from the southern Yukon indicate that the oxygen isotope composition of water from Jellybean Lake reflects the composition of mean-annual precipitation, δ18Op. Recent changes in the δ18O of Jellybean sedimentary calcite (δ18Oca) correspond to changes in the North Pacific Index (NPI), a measure of the intensity and position of the Aleutian Low (AL) pressure system. This suggests that δ18Op variability was related to the degree of fractionation during moisture transport from the Gulf of Alaska across the St. Elias Mountains and that Holocene shifts were controlled by the intensity and position of the AL. Following this model, between ∼7500 and 4500 cal yr B.P., long-term trends suggest a predominantly weaker and/or westward AL. Between ∼4500 and 3000 cal yr B.P. the AL shifted eastward or intensified before shifting westward or weakening between ∼3000 and 2000 cal yr B.P. Rapid shifts eastward and/or intensification occurred ∼1200 and 300 cal yr B.P. Holocene changes in North Pacific atmospheric circulation inferred from Jellybean Lake oxygen isotopes correspond with late Holocene glacial advances in the St. Elias Mountains, changes in North Pacific salmon abundance, and shifts in atmospheric circulation over the Beaufort Sea. 相似文献
323.
熊耳地体南侧中晚元古代地层碳氧同位素组成:CMF模式的证据 总被引:5,自引:9,他引:5
前人运用 CMF 模式(碰撞造山成岩成矿与流体作用模式)推断熊耳地体金银矿床的成矿流体主要来自其南侧中晚元古代地层(官道口群和栾川群)的陆内俯冲变质脱水作用,并推测该套地层富放射成因铅和锶,δ~(13)C 和δ~(18)O 值较高。为检验该推论和 CMF 模式正确与否,作者对该套地层开展了研究,本文报道了碳氧同位素研究结果。13件岩石样品δ~(18)O 值变化于9.1‰~16.7‰,平均13.3‰;4件δ~(13)C_(CaCO_3)值为-2.8‰~0.8‰,平均-0.9‰,计算表明,该套地层在320~373℃(熊耳地体多数矿床早阶段成矿温度范围)变质脱水所形成流体的δ~(18)O值为2.6‰~14.6‰,与推测结果一致,覆盖了熊耳地体已有早阶段成矿流体的δ~(18)O值(5.1‰~12.6‰),计算的中晚元古代地层变质流体的δ~(13)C_(CO_2)随介于-0.7‰~4‰,也与熊耳地体成矿流体的δ~(13)C_(CO_2)值(-2.1‰~4‰,成矿早阶段一般δ~(13)C_(CO_2)>0)一致。如此以来,我们的研究结果证明了前人的推论和 CMF 模式的科学性与实用性,CMF 模式可以用于指导熊耳地体或类似构造环境的矿床勘查和地质研究。 相似文献
324.
Isotope geochemistry of the mafic dikes from the Vazante nonsulfide zinc deposit, Brazil 总被引:2,自引:0,他引:2
M. Babinski L.V.S. Monteiro A.H. Fetter J.S. Bettencourt T.F. Oliveira 《Journal of South American Earth Sciences》2005,18(3-4):293-304
The Vazante Group, located in the northwestern part of Minas Gerais, hosts the most important zinc mine in Brazil, the Vazante Mine, which represents a major known example of a hypogene nonsulfide zinc deposit. The main zinc ore is represented by willemite and differs substantially from other deposits of the Vazante-Paracatu region, which are sulfide-dominated zinc-lead ore. The age of the Vazante Group and the hosted mineralization is disputable. Metamorphosed mafic dikes (metabasites) that cut the metasedimentary sequence and are affected by hydrothermal processes recently were found and may shed light on the geochronology of this important geological unit. Zircon crystals recovered from the metabasites are xenocrystic grains that yield U–Pb conventional ages ranging from 2.1 to 2.4 Ga, so the basement of the Vazante Group is Paleoproterozoic or has metasedimentary rocks whose source area was Paleoproterozoic. Pb isotopes determined for titanite separated from the metabasites have common, nonradiogenic Pb compositions, which prevents determination of their crystallization age. However, the Pb signatures observed for the titanite crystals are in agreement with those determined for galena from the carbonate-hosted Zn–Pb deposits hosted by the Vazante Group, including galena from minor sulfide ore bodies of the Vazante deposit. These similarities suggest that the metalliferous fluids that affected the metabasites may have been those responsible for galena formation, which could imply a similar lead source for both nonsulfide and sulfide zinc deposits in the Vazante–Paracatu district. This common source could be related to deep-seated, basin-derived, metalliferous fluids associated with a long-lived hydrothermal system related to diagenesis and deformation of the Vazante Group during the Neoproterozoic. 相似文献
325.
326.
327.
北印度洋季风研究的经典地区是上升流活跃的阿拉伯海和索马里海盆,孟加拉湾地区季风强弱的变化则是以浮游有孔虫壳体氧同位素值反映的淡水输入量大小来指示的.文章通过对孟加拉湾的MD77181岩芯的浮游有孔虫定量分析、氧碳稳定同位素分析,对比东经90°海岭的MD81349岩芯的同类分析结果,发现孟加拉湾地区在深海氧同位素2、3期出现上升流生物种丰度上升、表层水古生产力升高、表层水温度下降、温跃层变浅、盐度增加等指示存在上升流活动的现象,说明当时该区东北冬季风增强.特别的是间冰段深海氧同位素3期各古环境的代用指标都形成记录上最突出的峰值,且在同期背景值上叠加着强烈的波动,认为此现象应是印度季风区夏季季风和冬季季风强盛期的相互转换、水体的垂直循环运动等环境信号和控制机制在该区的反映. 相似文献
328.
Zuhair Kattan 《Hydrogeology Journal》2002,10(4):495-508
Groundwater from the Palaeogene aquifer system in north-eastern Syria has been studied using chemical and isotopic methods
to determine the effects of carbonate dissolution, sulphate reduction and geogenic CO2 incorporation in the dilution of 14C activity, and later to correct the conventional 14C water ages. The reason for this non-classical approach of correction is because the groundwater in this karstified and Nummulitic
carbonate aquifer occurs under confined and partly confined conditions, and is located in an area very close to deep faults
and fractures. Furthermore, the interconnection with the Upper Cretaceous formations, which commonly contain gypsum and hydrocarbons,
can facilitate the processes of sulphate reduction and geogenic CO2 incorporation, which should not be excluded. The dilution factor related to carbonate dissolution was estimated to be about
0.60–0.75. The dilution factor associated with sulphate reduction, which only depends on H2S content, was rather low (about 0.95). However, as a result of the local tectonic setting in this area, the influence of
geogenic CO2 incorporation was clearly high. The dilution factor associated with this effect ranges between 0.24–0.64. Consequently, the
corrected 14C ages are considerably reduced compared with those determined by classical models. Accordingly, the groundwater in the study
area can be divided into three main groups: (1) fresh, shallow and cold water of less than 1 ka age; (2) brackish, deep and
thermal water of rather old age (10.9–12.3 ka B.P.); and (3) an admixed groundwater of intermediate quality and age (1.9–6.7 ka B.P.).
Electronic Publication 相似文献
329.
南秦岭佛坪片麻岩系同位素年代学及其地质意义 总被引:10,自引:0,他引:10
佛坪片麻岩系是秦岭造山带核部所出露的众多古老块体之一,笔者利用锆石U-Pb法测得1853~2284Ma年龄数据,是目前该区所获最老年龄资料,可能接近于其成岩时代。其地质意义在于:①证实佛坪片麻岩成岩时代为早元古代;②424±5Ma、300±17Ma和212.8土9.4Ma的年龄信息表明加里东-印支期构造热事件对佛坪片麻岩有重大影响,③所获213.2~1447Ma等大量表面年龄数据是片麻岩长期演化过程中多次地质作用综合后的混合年龄。 相似文献
330.