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Fig.8e in our paper(Groves et al.,2018)was incorrectly ascribed to Caddey et al.(1995).It is actually taken from Figure 3 in Morelli et al.(2010).In turn,this was derived from Bell(2013).The authors apologise for this unintentional error. 相似文献
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《《地质学报》英文版》2001,75(3)
In recent years, fossils recognized as sponges and animal embryos have been reported in the Doushantuo phosphate rocks from the Guizhou Province(Li et al., 1998, Xiao et al., 1998). Zhang et al.(1998) disagreed with the interpretation of Li et al. that some of the needle-formed structures were monaxial spicules of sponges. They considered that these structures could be 相似文献
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榴辉岩中单斜辉石和石榴子石之间显著的镁同位素平衡分馏,使其成为一种具有潜力的高精度地质温度计。为此本文选取文献中已报道的来自西南天山洋壳冷俯冲造山带、大别-苏鲁陆壳碰撞造山带和南非卡普瓦尔克拉通三种构造环境中的64对单斜辉石—石榴子石矿物对镁同位素数据利用δ~(26)Mg_(Cpx)-δ~(26)Mg_(Grt)图解筛选出50对达到镁同位素平衡分馏的数据,采用Huang et al.(2013)通过第一性原理计算和Wang et al.(2012)、Li et al.(2016)分别通过经验估计得出的镁同位素温度计计算榴辉岩的峰期温度并与前人研究结果进行对比。通过分析计算结果发现对于造山带榴辉岩,Huang et al.(2013)的温度计计算结果与前人通过传统温度计和相平衡模拟研究结果较一致,较好地重现了榴辉岩的峰期温度,而Wang et al.(2012)和Li et al.(2016)的温度计计算结果明显低于前人获得的峰期温度;对于克拉通榴辉岩,三种镁同位素温度计的计算结果与前人通过传统温度计获得的研究结果大多数相差在50℃以上,很可能是早期退变质过程中镁同位素在高温条件下再平衡导致的这表明三种镁同位素温度计均不适用于克拉通榴辉岩。同时,基于这些榴辉岩样品数据,本文利用经验估计的方法进行校准,得到了新的单斜辉石-石榴子石镁同位素公式△~(26)Mg_(Cpx-Grt)=1.11×10~6/[T(K)]~2(R~2=0.92)。此外,本文也对单斜辉石-石榴子石镁同位素地质温度计的应用前景及应用时应当注意的问题进行了简单的探讨。 相似文献
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China Geological Survey Proved the Existence of an Extra-large Coal-Associated Lithium Deposit 总被引：2，自引：0，他引：2
SUN Yuzhuang 《《地质学报》英文版》2015,89(1):311-311
<正>The most Li deposits were found in lake waters or igneous rock.In recent years,anomalous concentrations of lithium in coal have been reported by several coal geologists(Sun et al.,2010,2012a,2013a;Dai et al.,2012).Some coal geologists argued that these concentrations have economic significance(Sun et al.,2012b,2013b,2014).This discovery has even been reported by Khanchuk et al.(2013)in"The Newsletter of Society for Organic Petrology",and the report was 相似文献
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浙江江山寒武系碳酸盐岩碳氧同位素特征及其古环境意义探讨 总被引：8，自引：1，他引：8
对浙江江山碓边下寒武统上部—下奥陶统下部碳酸盐岩进行了碳氧同位素测定。δ1 3C、δ1 8O值变化范围和均值分别为 - 1.9‰～ 3.7‰、- 13.0‰～ - 1.3‰和 0 .86‰、- 9.76‰。碳氧同位素地层曲线与 Veizer et al.(1986 )的同位素年代演化曲线形状相似 ,在寒武纪—奥陶纪界线附近没有明显的δ1 3C、δ1 8O漂移现象。δ1 3C地层曲线具旋回性变化特征 ,大陈岭组、杨柳岗组各形成一个完整的演化旋回 ,与根据露头层序地层研究推测的海平面变化曲线吻合性较好 ,表现出δ1 3C值的高值区是海盆水体变深的反映。一个明显的碳同位素正漂移发生于晚寒武世早期 (华严寺组下部 ) ,与 Matthew etal.(2 0 0 0 )报道的在美国内华达州中东部、哈萨克斯坦 Malyi Karatau地区、澳大利亚昆士兰州西北部和湘西桃源瓦儿岗等地发现的 δ1 3C正漂移记录 (SPICE— The Steptoean Positive CarbonIsotope Excursion)和 Veizer et al.(1986 )碳同位素年代演化曲线中的正漂移波峰一致 ,为晚寒武世全球性碳同位素正漂移提供了一个佐证。 相似文献
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<正>We thank Tan Mingxuan et al.(2017)for their comments stimulated by our short paper in the recent Acta Geologica Sinica(English edition).We are grateful for the opportunity to expand on the model of the supercritical hyperpycnal flow deposits in the Beilaishi section on the Lingshan Island,and to explain why the model proposed by Tan Mingxuan et al.(2017)cannot explain the bulk of 相似文献
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《吉林大学学报(地球科学版)》2015,(Z1)
<正>世界众多页岩气高产区Barnett、Fayetteville(Zumberge et al,2012)、Marcellus(Tilley et al,2013)、Haynesville(Ferworn et al,2008)、Albany Shale(Gao et al,2014)、Utica shales(Xia et al,1999;Xia et al,2012;Xia et al,2013)、Foothills(Tilley et al,2011)、Horn River(Tilley et al,2013)、鄂尔多斯盆地页 相似文献
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本文针对静力荷载作用的情况,对比了4种黏土中水平受荷大直径单桩的设计方法,包括基于p-y弹簧模型的API规范方法,以及新近发展的基于p-y弹簧模型的Zhang et al.(2017b) 、基于双弹簧模型的Wang et al.(2020) 方法以及基于三弹簧模型的Fu et al.(2020) 方法。考虑两种大直径单桩常用的长径比(L/D=5和10),通过与三维有限元结果比较,对现有设计方法进行了对比,分析了不同参数对预测结果的影响。结果表明:(1)对于大直径单桩的水平位移和转角,现行API规范的预测值最大,而Wang et al.(2020) 方法预测值最小; (2)Fu et al.(2020) 方法不仅考虑了桩底剪力及桩身摩擦造成的分布力矩,还能够有效捕捉初始剪切模量与土体延性对水平响应的影响,还因此具备其余方法所不具备的优势; (3)采用Fu et al.(2020) 方法时,桩土界面粗糙系数α越大,桩身位移与转角越大,且长径比越小影响越显著,而与桩身分布力矩有关的缩放系数ξp2的影响则相对有限,当L/D≥10时其影响可以忽略。 相似文献
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INTRODUCTIONA suite of strongly deformed and metamor-phosed banded-augen (rapakivi) anatectic granitoids(charnockite) can be found at Dongzhen, Sihe ,Heshui and Baishi in Xinyi County , Changpo ,Gaozhou, Yunlu and Huanglingin Gaozhou County ,western Guangdong Province and Liuma , Tiantang-shan mountain in Luchuan County , and easternGuangxi in the Yunkai orogenic belt . Research onthe genesis and chronology of the granitoids has beenconducted by Mo et al . (1980) and Lin et al .(1… 相似文献
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ZHAO Yong 《《地质学报》英文版》2018,92(4):1676-1677
正Objective LGM is a critical climate period in the late Quaternary and is the most recent extreme cold event.Clark et al.(2009)used 4271 14C records and 475 cosmogenic nuclide datings to define LGM be in 26.5–19.0 ka BP.LGM age often changes with time in different regions(Mix et al.,2001;Zhang Zhigang et al.,2015).However,LGM has not been described to date in the Beijing region.During our field work in 2015–2017,LGM event stratigraphy was 相似文献
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By using the numerical method to model the ter-rain effect on the magnetotelluric field,few resultshave been obtained. The finite element method(FEM) was used by Chouteau and Bouchard (1988)and Wannamaker et al .(1986) ,andthe boundary el-ement method (BEM) was used by Xu and Zhou(1997) and Xu (1995) to model 2Dtopographyinflu-ences on magnetotelluric surveys . The BEM methodwas also used to model the 3Dtopographic effect onmagnetotelluric deep sounding (Xu et al .,1997 ;Xu,1995) .In t… 相似文献
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CHEN Bin LIU Shuwen WANG Rui CHEN Zhichao LIU Chaoqun Key Laboratory of Orogenic Belts Crustal Evolution MOE School of Earth Space Sciences Peking University Beijing 《《地质学报》英文版》2006,80(6)
1 Introduction The tectono-thermal evolution of the North China Craton (NCC) in Late Archean to Paleoproterozoic times has long been attractive to many researchers (Wan et al., 2000; Zhao et al., 2000, 2002; Guo et al., 2001; Liu et al., 2002; Zhai and Liu 2003; Zhai, 2004; Yu et al., 2004; Kr?ner et al., 2005; Wilde et al., 2005). Zhao et al. (2000, 2002) proposed a tectono-thermo framework for the evolution of the NCCbased on detailed petrological and geochronological data, and they … 相似文献