Metamorphic olivine after dehydration embrittlement in Serpentinite: Case study from the Shiraga Serpentinite mass in the Sanbagawa high P/T metamorphic belt,central Shikoku,Japan     

Seiya Fukumura  Kazuaki Okamoto  Masaru Terabayashi 《Island Arc》2019,28(2)

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Cometary outbursts – search of probable mechanisms – case of 29P/Schwassmann‐Wachmann 1     

P. Gronkowski 《Astronomische Nachrichten》2002,323(1):49-56

Cometary outbursts, sudden increases in luminosity have not been clearly explained so far and their source is still a mystery. Various possible mechanisms as a source of cometary outbursts at large distances from the Sun have been considered. It has been stated that plausible mechanisms are the polymerization of HCN and the amorphous water ice transformation combined with electrostatic destruction of cometary grains in the head of the comet. The calculations have been carried out for a large range of cometary parameters and it has been shown that the proposed scenario of the outburst gives a jump in the comet brightness which is consistent with the real jump observed during the 29P/Schwassmann‐Wachmann 1 outbursts.  相似文献   

远震P波层析成像研究阿尔金断裂带东端及其邻区深部结构   总被引：3，自引：1，他引：2       下载免费PDF全文

邹长桥  贺日政  段永红  魏运浩  刘巧霞  刘洋 《地球物理学报》2017,60(6):2279-2290

本文利用"中国地震科学台阵探测——南北地震带北段"项目在内蒙古阿拉善西部及甘肃西北部地区布设的80个流动宽频带地震仪及16个固定台站,于2013年10月—2015年6月所记录的787个远震事件,采用波形相关方法拾取了共49052个高质量的P波走时残差数据,并利用Fast-Marching远震走时层析成像方法,反演获取了研究区下方的三维P波速度结构.结果显示:阿尔金断裂带东段、祁连山、北山地区下方地壳结构表现为低速异常特征,具有明显的造山带构造特征;阿拉善地体下方地壳结构表现为高速异常特征,为典型的大陆地壳结构特征;阿拉善地块沿着青藏高原北边界逆冲断裂(NBT)南向俯冲,其在祁连山造山带下与北向俯冲的柴达木岩石圈形成了面对面的碰撞接触关系;阿尔金断裂带的末端并没有北东向延伸到阿拉善块体,而是受到刚性的阿拉善岩石圈阻挡沿着其南缘断裂带继续向东发展.  相似文献   

藏北申扎羊湖河谷140ka B.P.以来古环境的初步研究   总被引：7，自引：0，他引：7       下载免费PDF全文

刘爱民  喻建新  贺永忠  卢定彪  牟世勇  岳龙  杨家禄 《第四纪研究》2003,23(1):83-91

通过对藏北羊湖河谷第四纪沉积成分、地貌、年龄值、孢粉和氧化物等的测试、研究,确定了本区140kaB.P.以来沉积序列和1个河流阶地、3个河湖积台地的地貌状况,并得到140kaB.P.以来本区至少经历了4个半干-湿气候旋回,目前正处于干旱期.同时通过不同时期的阶地、台地的不同高程使我们得以了解地壳相对抬升趋势,从98.5kaB.P.以来地壳抬升速率为2.21mm/a,总体显示抬升速率低的特征.  相似文献   

利用P波初动及振幅比初步计算2005年11月26日九江-瑞昌地震余震震源机制     

杨中书  李超 《华南地震》2006,26(3):77-82

应用Jeanne L.Hardebeck和Peter M.Shearer编制的利用P波初动和振幅比计算地震震源机制解的程序,使用九江-瑞昌流动地震台观测的地震资料,初步计算了九江-瑞昌地震余震的震源机制;并对单独利用P波初动和利用初动及振幅比这两种计算方法进行了比较.综合最优计算结果,九江-瑞昌地震余震震源机制解为:走向174°,倾角62°,滑动角43°.  相似文献   

甲醛对南美白对虾(Penaeus vannamei)β-N-乙酰-D-氨基葡萄糖苷酶的失活动力学研究   总被引：2，自引：0，他引：2  

谢晓兰  石艳  黄乾生  陈清西 《海洋通报(英文版)》2006,8(1):34-45

β-N-乙酰-D-氨基葡萄糖苷酶与南美白对虾的食物消化吸收、蜕壳生长有着密切关系。海水里存在的有机污染物将影响酶生理功能,从而进一步影响虾的正常蜕壳,严重将导致对虾的死亡。甲醛是常用的有机溶剂,故本文应用动力学方法研究了南美白对虾β-N-乙酰-D-氨基葡萄糖苷酶在甲醛溶液中以 pNP-NAG为底物时酶活力的变化规律。表明酶在甲醛浓度低于 2.0 mol?L-1,酶的失活过程是可逆的,测得甲醛对酶抑制的 IC50为 1.05 mol?L-1。用双倒数作图法测定甲醛对酶的抑制类型,结果显示甲醛是酶的竞争性抑制剂,甲醛只能与游离酶(E)结合,底物对酶的失活具有保护作用。用底物反应动力学方法观测在不同底物浓度下酶在 0.0、0.5、1.0、1.5、2.0 mol?L-1 的醋酸酐溶液中的失活过程,分别测定了酶的微观失活速度常数 k 0及复活速度常数 k-0 并加以比较,结果表明甲醛对酶的影响是缓慢结合同时导致失活的过程,比较微观失活速度常数 k 0 及复活速度常数 k-0,结果暗示在高浓度的甲醛溶液中,酶将完全失活。  相似文献   

Early Carboniferous HP metamorphism in the Hida Gaien Belt,Japan: Implications for the Palaeozoic tectonic history of proto‐Japan     

Takumi Yoshida  Tomoki Taguchi  Hayato Ueda  Kenji Horie  M. Satish‐Kumar 《Journal of Metamorphic Geology》2021,39(1):77-100

We report two new eclogite localities (at Kanayamadani and Shinadani) in the high‐P (HP) metamorphic rocks of the Omi area in the western most region of Niigata Prefecture, Japan, which form part of the Hida Gaien Belt, and determine metamorphic conditions and pressure–temperature (P–T) paths. The metamorphic evolution of the eclogites is characterized by a tight hairpin‐shaped P–T path from prograde epidote–blueschist facies to peak eclogite facies and then retrograde blueschist facies. The prograde metamorphic stage is characterized by various amphibole (winchite, barroisite, glaucophane) inclusions in garnet, whereas the peak eclogite facies assemblage is characterized by omphacite, garnet, phengite and rutile. Peak P–T conditions of the eclogites were estimated to be ~600°C and up to 2.0 GPa by conventional cation‐exchange thermobarometry, Ti‐in‐zircon thermometry and quartz inclusion Raman barometry respectively. However, the Raman spectra of carbonaceous material thermometry of metapelites associated with the eclogites gave lower peak temperatures, possibly due to metamorphism at different conditions before being brought together during exhumation. The blueschist facies overprint following the peak of metamorphism is recognized by the abundance of glaucophane in the matrix. Zircon grains in blueschist facies metasedimentary samples from two localities adjacent to the eclogites have distinct oscillatory‐zoned cores and overgrowth rims. Laser ablation inductively coupled plasma mass spectrometry U–Pb ages of the detrital cores yield a wide range between 3,200 and 400 Ma, with a peak at 600–400 Ma. In the early Palaeozoic, proto‐Japan was located along the continental margin of the South China craton, providing the source of the older population of detrital zircon grains (3,200–600 Ma) deposited in the trench‐fill sediments. In addition, subduction‐related magmatism c. 500–400 Ma is recorded in the crust below proto‐Japan, which might have been the source for the younger detrital zircon grains. The peak metamorphic age was constrained by SHRIMP dating of the overgrowth rims, yielding Tournaisian ages of 347 ± 4 Ma, suggesting subduction in the early Carboniferous. Our results provide clear constraints on the initiation of subduction, accretion and the development of an arc‐trench system along the active continental margin of the South China craton and help to unravel the Palaeozoic tectonic history of proto‐Japan.  相似文献   

Late‐stage orogenic loading revealed by contact metamorphism in the northern Appalachians,New York     

K. M. Dorfler  R. J. Tracy  M. J. Caddick 《Journal of Metamorphic Geology》2014,32(1):113-132

Pelitic schists from contact aureoles surrounding mafic–ultramafic plutons in Westchester County, NY record a high‐P (~0.8 GPa) high‐T (~790 °C) contact overprint on a Taconic regional metamorphic assemblage (~0.5 GPa). The contact metamorphic assemblage of a pelitic sample in the innermost aureole of the Croton Falls pluton, a small (<10 km²) gabbroic body, consists of quartz–plagioclase–biotite–garnet–sillimanite–ilmenite–graphite–Zn‐rich Al‐spinel. Both K‐feldspar and muscovite are absent, and abundant biotite, plagioclase, sillimanite, quartz and ilmenite inclusions are found within subhedral garnet crystals. Unusually low bulk‐rock Na and K contents imply depletion of alkalic components and silica through anatexis and melt extraction during contact heating relative to typical metapelites outside the aureole. Thermobarometry on nearby samples lacking a contact overprint yields 620–640 °C and 0.5–0.6 GPa. In the aureole sample, WDS X‐ray chemical maps show distinct Ca‐enriched rims on both garnet and matrix plagioclase. Furthermore, biotite inclusions within garnet have significantly higher Mg concentration than matrix biotite. Thermobarometry using GASP and garnet–biotite Mg–Fe exchange equilibria on inclusions and adjacent garnet host interior to the high‐Ca rim zone yield ~0.5 ± 0.1 GPa and ~620 ± 50 °C. Pairs in the modified garnet rim zone yield ~0.9 ± 0.1 GPa and ~790 ± 50 °C. Thermocalc average P–T calculations yield similar results for core (~0.5 ± ~0.1 GPa, ~640 ± ~80 °C) and rim (~0.9 ± ~0.1 GPa, ~800 ± ~90 °C) equilibria. The core assemblages are interpreted to record the P–T conditions of peak metamorphism during the Taconic regional event whereas the rim compositions and matrix assemblages are interpreted to record the P–T conditions during the contact event. The high pressures deduced for this later event are interpreted to reflect loading due to the emplacement of Taconic allochthons in the northern Appalachians during the waning stages of regional metamorphism (after c. 465 Ma) and before contact metamorphism (c. 435 Ma). In the absence of contact metamorphism‐induced recrystallization, it is likely that this regional‐scale loading would remain cryptic or unrecorded.  相似文献   

Micro‐sampling Lu–Hf geochronology reveals episodic garnet growth and multiple high‐P metamorphic events          下载免费PDF全文

H. Cheng  X. C. Liu  J. D. Vervoort  D. Wilford  D. D. Cao 《Journal of Metamorphic Geology》2016,34(4):363-377

We present Lu–Hf dates from multiple growth zones within two large garnet porphyroblasts by a micro‐sampling method. A single eclogite sample, taken from the Huwan shear zone in the Hong'an orogen, was investigated with Lu–Hf geochronology by micro‐sampling and traditional bulk separation methods. The sample contains a few large garnet porphyroblasts up to several centimetres in diameter and a second major population of smaller (0.1–2.0 mm) garnet porphyroblasts, comprised of dark cores and pale rims. Elemental compositions and mineral inclusions in the garnet appear consistent with two garnet generations. Lu–Hf dates (c. 400–264 Ma) were determined from twelve micro‐sawed garnet sections from two large garnet porphyroblasts. These Lu–Hf dates overlap with age peaks defined by 115 SIMS zircon U–Pb analyses from the same eclogite sample. Bulk analyses of smaller garnet separates define a minimum date of c. 306 Ma and a maximum date of c. 252 Ma for the dark cores and pale rims respectively. These Lu–Hf dates were interpreted to bracket the period of garnet growth and the broad interval from c. 400 to 264 Ma is best explained by protracted and episodic garnet growth, which may require that these rocks experienced two subduction cycles that were initiated during the Devonian and terminated in the Triassic.  相似文献   

基于P2P和QoS的移动GIS地图服务模型研究     

王柯  张文诗  康鑫  马宏斌 《地理信息世界》2015,(1)

介绍了移动GIS地图服务应用发展及趋势;研究了移动GIS地图服务中对等网络和地图服务质量控制机制的构建方法;基于P2P技术和QoS技术,针对移动GIS地图服务应用中存在的一些弊病,提出了四种服务模型：数据分层分块模型、地图服务匹配模型、数据缓存下载模型和地图数据传输模型,这些模型对于移动GIS地图服务应用中理论研究和技术开发具有较高的参考价值和借鉴意义。  相似文献