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91.
滦家河花岗岩体是胶东金矿区内的重要岩体,其岩性主要为中粗粒黑云母二长花岗岩。锆石LA—ICP—MS U—Pb年代学研究表明,滦家河花岗岩形成于149±2 Ma,属晚侏罗世。滦家河花岗岩Si O2的含量为64.58%~72.05%,相对较高;A/CNK值为0.98~1.22。微量元素特征显示,滦家河花岗岩富集大离子亲石元素(LILE)Rb、Ba、K,强烈亏损高场强元素(HFSE)Nb、Ta、Ti、P;稀土元素特征显示轻稀土强烈富集,重稀土极度亏损,轻微正铕异常。岩石的Nb/La和Nd/Th比值显示壳源花岗岩的特征,Rb/Sr比值暗示可能有部分幔源物质混入。结合区域地质分析认为,侏罗纪开始,太平洋板块向欧亚大陆的俯冲引发大规模幔源岩浆底侵,导致地壳物质部分熔融形成滦家河花岗岩。 相似文献
92.
桂东鹰扬关群火山岩时代和构造环境的重新厘定:对钦杭结合带西南段构造格局的制约 总被引:2,自引:0,他引:2
鹰扬关群在湘—粤—桂三省交界地区广泛发育,为一套以绿片岩相变质的细碧岩、(石英)角斑岩及相关的火山碎屑岩为主,含有细碎屑岩和碳酸盐岩组合。该群的成岩背景过去一直认为是Rodinia超大陆裂解背景下的大陆裂谷环境,时代归属为新元古代。岩石学、地球化学和锆石LA-ICP-MS U-Pb定年结果表明,鹰扬关群火山岩主要属于基性-中性火山(碎屑)岩类,在岩石化学成分上表现为明显富集大离子亲石元素(LILE,包括U、Th、Ba、K和Rb等)和轻稀土元素,而Nb、Ta、P和Ti等高场强元素和重稀土元素相对亏损,反映其具有俯冲-消减作用形成的岛弧-弧后盆地型火山岩地球化学特征;获得鹰扬关群中变角斑岩的锆石LA-ICP-MS U-Pb谐和年龄为(415.1±2.1)Ma(n=13,MSWD=1.8),表明其为加里东期海相火山喷发的产物。结合云开地块北缘存在有早古生代MORB型和岛弧型变质基性火山岩的资料表明,扬子板块和华夏板块结合带(称之为钦—杭结合带)西南段有早古生代的古洋盆,鹰扬关群岛弧-弧后盆地型火山岩可能是钦—杭结合带南西段早古生代洋陆俯冲-消减过程的地质记录,钦—杭结合带西南段加里东期的构造格局是俯冲增生造山带而不是陆内造山带。 相似文献
93.
High‐resolution reconstruction of a coastal barrier system: impact of Holocene sea‐level change 下载免费PDF全文
Mikkel Fruergaard Thorbjørn J. Andersen Lars H. Nielsen Peter N. Johannessen Troels Aagaard Morten Pejrup 《Sedimentology》2015,62(3):928-969
This study presents a detailed reconstruction of the sedimentary effects of Holocene sea‐level rise on a modern coastal barrier system. Increasing concern over the evolution of coastal barrier systems due to future accelerated rates of sea‐level rise calls for a better understanding of coastal barrier response to sea‐level changes. The complex evolution and sequence stratigraphic framework of the investigated coastal barrier system is reconstructed using facies analysis, high‐resolution optically stimulated luminescence and radiocarbon dating. During the formation of the coastal barrier system starting 8 to 7 ka rapid relative sea‐level rise outpaced sediment accumulation. Not before rates of relative sea‐level rise had decreased to ca 2 mm yr?1 did sediment accumulation outpace sea‐level rise. From ca 5·5 ka, rates of regionally averaged sediment accumulation increased to 4·3 mm yr?1 and the back‐barrier basin was filled in. This increase in sediment accumulation resulted from retreat of the barrier island and probably also due to formation of a tidal inlet close to the study area. Continued transgression and shoreface retreat created a distinct hiatus and wave ravinement surface in the seaward part of the coastal barrier system before the barrier shoreline stabilized between 5·0 ka and 4·5 ka. Back‐barrier shoreline erosion due to sediment starvation in the back‐barrier basin was pronounced from 4·5 to 2·5 ka but, in the last 2·5 kyr, barrier sedimentation has kept up with and outpaced sea‐level. In the last 0·4 kyr the coastal barrier system has been prograding episodically. Sediment accumulation shows considerable variation, with periods of rapid sediment deposition and periods of non‐deposition or erosion resulting in a highly punctuated sediment record. The study demonstrates how core‐based facies interpretations supported by a high‐resolution chronology and a well‐documented sea‐level history allow identification of depositional environments, erosion surfaces and hiatuses within a very homogeneous stratigraphy, and allow a detailed temporal reconstruction of a coastal barrier system in relation to sea‐level rise and sediment supply. 相似文献
94.
Cosmic ray exposure ages of frost-weathered bedrock from mountain summits in the Outer Hebrides exceed the age of Late Devensian glaciation. Exposure ages of most glacially-abraded bedrock surfaces at low and intermediate elevations are younger than the age of maximum Late Devensian glaciation. These results confirm that previously mapped periglacial trimlines in the Outer Hebrides define the upper limit of bedrock erosion by Late Devensian ice. They are consistent with the interpretation, based on geomorphological evidence, that the trimlines mark the approximate upper limit of a Late Devensian Outer Hebrides Ice Cap. A postglacial exposure age from the summit of Oreval (662 m) suggests that this mountain was overrun during the last glaciation, indicating thicker ice cover and a lower surface gradient west of the ice-cap divide than previously inferred. Although bedrock surfaces below the trimlines are strongly ice-moulded, some show evidence of prior cosmic ray exposure, which we attribute to limited erosion during Late Devensian glaciation. If this interpretation is correct, the youngest apparent ages from these surfaces give the most reliable dates for deglaciation, at ca. 14.5–14 ka. This implies that ice persisted at favourable sites through the warm opening phase of the Windermere Interstade. Comparison with radiocarbon-dated evidence from offshore cores suggests net ice margin retreat of ∼74 km eastwards across the adjacent shelf in > 2.3 ± 1.0 ka. The dating evidence is consistent with relatively rapid retreat of calving margins to the coast, then slower withdrawal of ice margins to high ground. Copyright © 2005 John Wiley & Sons, Ltd. 相似文献
95.
古本《竹书纪年》记载有:“周昭王十九年,天大噎,雉兔皆震,丧六师于汉。”这与阴天发生的日全食现象十分相似。事件发生在昭王末年南征荆楚的过程中,地点应当在从周都到洞庭湖以南之间的某处。由前人的研究可知昭王十九年应在公元前1010。940年之间。在充分讨论了天文计算的不确定性后得到这一地区可见的9次大食分日食,其中公元前1009和976年的两次日食可能在洞庭湖以南造成日全食,其他地点也都有相当大的食分。在对夏商周断代工程得到的西周年表作微小调整后,昭王十九年天大睦可以认定为公元前976年5月31日日全食。这对“夏商周断代工程”所定出的昭王前后年代是一个独立的支持。 相似文献
96.
97.
A 14C-dated magnetostratigraphy of absolute declination and inclination between 12500 and 10000 14C yr BP was recently developed for southern Sweden. Recently also the Swedish geochronological time-scale, based on c. 11 500 annually deposited clay-varves, was connected with the present. It should therefore be possible to compare the two chronologies with a reliable magnetostratigraphic record in an appropriate clay-varve section. We have found such a site within the Middle Swedish end-moraine zone. Statistical correlations between the two independently dated time-scales suggest that at 10500–10200 14Cy r BP the varve chronology exceeds the 14C chronology by the order of 500-600 varve yr. Other correlations indicate that the difference between the two chronologies was less at 11000 14C yr BP, and further correlations between the time-scales at 12000 14C yr BP suggest that the difference between the chronologies increased steadily from 12000 to 10000 14C yr BP. If these correlations are correct they imply that the 14C production rate increased steadily during the Late Weichselian. 相似文献
98.
用天文方法建立商后期甲骨文年代序列的新途径—解析殷历月法 总被引:8,自引:2,他引:6
利用对具有月龄特征的历谱规律的研究成果,以推定甲骨文的绝对年代,从而提供了建立商后期甲骨文年代序列的新方法,并给出了13版卜辞的例证,通过分析殷历月的结构,得出殷历中“二癸月”和“四癸月”的月首分别为首甲日和首癸日,初步归纳出殷历月法,月首为初三,月长等于逆望月周期,建立固定,且找到建立丑之例,置闰规律未知,已存在年终,年中置闰两种闰法。 相似文献
99.
Lubbock Lake (Southern High Plains of Texas) contains a cultural, faunal, and floral record within a virtually complete geological record spanning the past 11 100+ years. More than 88 archaeological occurrences have been excavated from five major stratigraphic units. The Paleoindian record (11 500–6500yr BP) begins with Clovis-age occupation (ca. 11 100yr BP) found within fluvial deposits (stratum 1). Subsequent Paleoindian occupations are found in lake and marsh sediments (stratum 2). Archaic occupations (8500-2000yr BP) are contained within aeolian and marsh deposits (strata 3 and 4). Ceramic occupations (2000-500yr BP) are found on a soil developed in stratum 4, in marsh sediments (strata 4 and 5), and in slopewash and aeolian sediments (stratum 5). The Protohistoric (500-300yr BP) and Historic (300-100yr BP) remains are in slopewash, aeolian, and marsh sediments (stratum 5) and associated soils. The Southern High Plains remained a grasslands throughout the last 11 500 years and neither man nor bison abandoned the region. The successive local faunas reflect changing ecosystems under pluvial to arid to more mesic to semiarid conditions. The occupation of Lubbock Lake through time appears to have been by small groups of people for both economic and short-term residential uses. These hunter-gatherer peoples underwent adaptive change brought about by climatic stress and alterations to food resources. 相似文献
100.
Our two newly obtained high-quality 40Ar/39Ar ages suggest that the high-K volcanic rocks of the Lawuxiang Formation in the Mangkang basin, Tibet were formed at 33.5
± 0.2 Ma. The tracing of elemental and Pb-Sr-Nd isotopic geochemistry indicates that they were derived from an EM2 enriched
mantle in continental subduction caused by transpression. Their evidently negative anomalies in HFSEs such as Nb and Ta make
clear that there is an input of continental material into the mantle source. The high-K rocks at 33.5 ± 0.2 Ma in the Mangkang
basin may temporally, spatially and compositionally compare with the early one of two-pulse high-K rocks in eastern Tibet
distinguished by Wang J. H. et al., implying that they were formed in the same tectonic setting. 相似文献