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西南天山晚古生代后碰撞岩浆作用：以阔克萨彦岭地区巴雷公花岗岩为例 总被引：8，自引：0，他引：8
西南天山阔克萨彦岭地区巴雷公钾长花岗岩出露于蛇绿混杂岩南侧。地球化学特征显示，该岩石富碱（K2O＋Na2O为8.25～8.72％〉8％），富钾（K2O／Na2O为1.34～1.56），准铝质（A／CNK为0.94～1.05），为高钾钙碱性-钾玄岩系列；岩石富集大离子亲石元素和轻稀土，亏损Sr、P等大离子亲石元素及Nb、Ti等高场强元素，具有中等的负铕异常（δEu=0.49～0.59），为向A型花岗岩过渡的后碰撞高钾花岗岩特征；岩石的Nd／Th（1.64～3.19）、Th／U（5.95～7.11）、Nb／Ta（7.26～9.17）和高K2O／Na2O比值、低Sr／Ba比值特征表明，巴雷公花岗岩来源于中下地壳物质的部分熔融，残留相为斜长角闪岩。阴极发光图像显示，该岩石中锆石多呈完好的自形晶，具有岩浆锆石特有的韵律环带结构，LA-ICP-MS微区原位U-Pb定年结果表明该花岗岩的结晶侵位年龄为273±2Ma。综合南天山已有研究成果，推测南天山造山带后碰撞花岗质岩浆活动主要发生在282～259Ma之间，具有从高钾钙碱系列（282～266Ma）向碱性系列（266～259Ma）演化的特征，暗示了一个后碰撞阶段的造山带垮塌、陆壳连续伸展减薄的过程。巴雷公高钾花岗岩应为南天山造山带碰撞造山峰期变质后垮塌过程中的第一个阶段或碰撞造山到后造山的一个转折阶段的中下地壳熔融的产物，指示南天山西段古洋盆在中二叠世以前已经闭合，西南天山已进入后碰撞演化阶段，代表了古亚洲洋南部的闭合和中亚南部增生造山作用的结束。这一认识为深入探讨中亚后碰撞岩浆作用的时限和机制提供了新的约束资料。 相似文献
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在霍普金森试验系统上进行了花岗岩破坏的动静组合加载实验,根据实验结果,分析了岩石在动静组合加载下损伤断裂机制与特征.结果表明,不同动静组合加载下岩石破碎的粒度分布具有明显的率变效应;采用张开位移法计算出了岩石破裂时裂纹的宽度. 相似文献
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新疆东准噶尔地区的萨惹什克锡矿呈脉状产于萨北花岗岩体中。对于这种脉状矿床，成岩和成矿近时性的时间制约是证明矿床与围岩有成因关系的首要证据。萨北岩体由含碱性铁镁矿物的碱性花岗岩组成，全岩地球化学结果显示，碱性花岗岩具高碱、低Ca，明显富集稀土元素、高场强元素（zr，Hf，Nb，Ta，Y）和大离子亲石元素（Rb，Th，U），而强烈亏损Sr，Ba，Eu，属于典型的碱性A型花岗岩。锡矿脉由占绝对优势的锡石和石英组成，受北东和近东西向的断裂破碎带控制。原有研究证实，形成该锡矿床的成矿流体属于具高温、低盐度和低密度的岩浆水。据此并结合锡矿体的围岩性质，前人认为锡矿床与碱性花岗岩有成因联系。但是，由于分析技术和样品选择上的制约，萨北岩体成岩和萨惹什克锡矿成矿的确切时代一直没有得到合理的解决。本文报道了我们最近获得的碱性花岗岩锆石IA-ICP-MS U-Pb和锡矿石辉钼矿Re-0s同住素年龄（分别为306±3Ma和307±11Ma）。上述结果表明，萨北碱性花岗岩和萨惹什克锡矿石属于同期地质事件的产物，从而为两者具有密切成因联系提供了重要的年代学制约。此外，根据碱性花岗岩的БNd（t）（=＋5.0）低于研究区亏损地幔4.5个Б单位，我们认为形成萨北岩体的花岗岩浆不是直接来源于亏损地幔玄武质岩浆结晶分异作用的产物，而更可能是起源于本区年轻洋壳和陆源沉积物的部分熔融。 相似文献
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北秦岭西段新元古代两河口岩体,岩性为眼球状片麻状二长花岗岩,含少量黑云母、角闪石及榍石,属钾质钙碱性花岗岩类;主量元素SiO2=68.48%～72.45%,K2O/Na2O=1.35～2.07,为钾质;在K2O～SiO2关系图上投入高钾钙碱性区;A/CNK介于1.03～1.31,总体为钾质钙碱性弱过铝质花岗岩.岩石富集LILE元素（K、Th、Rb、Ba等）,亏损HFSE元素（Ta、Nb、Y、Yb等）;稀土元素总量较高（ZREE=126.82×10^-6～267.359×10^-6）,轻重稀土强烈分馏（∑LREE/∑HREE=5.447～8.894）,稀土元素分配模式为轻稀土富集型,具中等程度Eu负异常（δEu=0.417～0.621）.微量、稀土元素分配模式与北秦岭东部的碰撞型德河岩体、寨根岩体及牛角山岩体一致.Pb-Sr-Nd同位素组成具低的εNd=-3.9180～-6.0064、较高的87Sr/86Sr（t）=0.70760～0.71675、富放射性成因Pb同位素组成,模式年龄tDM=1849.73～2022.79Ma,指示两河口岩体源岩特征与秦岭岩群、马衔山群相近,岩浆源区为下地壳成因.结合区域资料,认为两河口岩体形成于同碰撞末期-后碰撞初期的构造转换时期;这一认识细化了北秦岭新元古代碰撞造山过程;其所确立的汇聚碰撞时间与我国晋宁运动时限一致;为研究中国古陆块在新元古代时期汇聚时限、过程、方式及Rodinia超大陆事件在秦岭地区的响应提供了重要证据. 相似文献
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张平祥 《石家庄职业技术学院学报》2012,24(6):9-11
引用广州地铁萝香区间盾构机掘进通过花岗岩球状风化体的案例,对盾构穿越花岗岩球状风化体发育地层的施工风险进行了分析.在施工过程中,采取盾构机掘进参数控制、同步注浆控制、施工监测与二次补充注浆的方法,成功通过花岗岩球状风化体.列举了一些施工中的异常情况和处理措施. 相似文献
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Experiments and sensitivity analyses for heat transfer in a meter-scale regularly fractured granite model with water flow 总被引：1，自引：0，他引：1
Experiments of saturated water flow and heat transfer were conducted for a meter-scale model of regularly fractured granite. The fractured rock model (height 1502.5 mm, width 904 mm, and thickness 300 mm), embedded with two vertical and two horizontal fractures of pre-set apertures, was constructed using 18 pieces of intact granite. The granite was taken from a site currently being investigated for a high-level nuclear waste repository in China. The experiments involved different heat source temperatures and vertical water fluxes in the embedded fractures either open or filled with sand. A finite difference scheme and computer code for calculation of water flow and heat transfer in regularly fractured rocks was developed, verified against both the experimental data and calculations from the TOUGH2 code, and employed for parametric sensitivity analyses. The experiments revealed that, among other things, the temperature distribution was influenced by water flow in the fractures, especially the water flow in the vertical fracture adjacent to the heat source, and that the heat conduction between the neighboring rock blocks in the model with sand-filled fractures was enhanced by the sand, with larger range of influence of the heat source and longer time for approaching asymptotic steady-state than those of the model with open fractures. The temperatures from the experiments were in general slightly smaller than those from the numerical calculations, probably due to the fact that a certain amount of outward heat transfer at the model perimeter was unavoidable in the experiments. The parametric sensitivity analyses indicated that the temperature distribution was highly sensitive to water flow in the fractures, and the water temperature in the vertical fracture adjacent to the heat source was rather insensitive to water flow in other fractures. 相似文献
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外墙花岗岩干挂是近几年的新的施工工艺。克服了石材饰面外表不同程度出现瘢痕、析白“泪痕”,还具有防潮、隔热、强度高、耐腐蚀、稳定可靠、可连续作业等特点。 相似文献
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Slađana Popović Nikola Unković Gordana Subakov Simić Milica Ljaljević Grbić 《文物保护研究》2018,63(5):292-302
The presence of biofilms on stone monuments can lead to biodeterioration processes that significantly lower not only the aesthetic value of cultural heritage sites but also cause considerable physical and chemical damage to stone surfaces. In terrestrial environments, cyanobacteria have a significant role in biofilm formation on a variety of natural and artificial stone substrata, including granite, sandstone, limestone, lime mortar, etc. Studies on cyanobacterial diversity and estimation of biodeteriorative activity on stone cultural heritage objects can be very important for conservators and restorers, and cyanobacteria removal from stone monuments is currently a great challenge for conservation science. In that sense, the diversity of terrestrial cyanobacteria was investigated at six localities in Serbia. Samples for cyanobacterial analyses were taken from surface biofilms covering different substrata: granite and lime mortar (The Monument to the Unknown Hero), sandstone (Branko's Bridge, Eiffel’s Lock) and carbonate rock (Medieval tombstones from Mramorje and Rasti?te, Gradac Monastery). A total of 18 cyanobacterial taxa were identified. The highest diversity was found on carbonate rock, followed by sandstone. Cyanobacteria were also recorded on an artificial substratum – lime mortar, while cyanobacteria were not found on granite. All detected cyanobacteria seriously impaired the structural and aesthetic integrity of the studied monuments via mechanical and chemical actions, so their presence must not be overlooked. 相似文献
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东海片麻状碱性花岗岩是扬子克拉通北东缘最具代表性的含碱性铁镁矿物的过碱性A型花岗岩.高精度的LA-ICP-MS锆石U-Pb定年结果表明,这些岩石形成于新元古代中期770Ma左右,并在约250Ma时经历超高压变质作用,之后又于210Ma左右遭受了大规模的角闪岩相退变质作用的改造.Nd同位素示踪表明东海片麻状碱性花岗岩具有相对偏高的εNd（t）值（＋1.4～-5.91）,指示其应是成熟度较低的下地壳部分熔融的产物,但不排除部分岩体在成岩过程中可能有少量幔源物质卷入.综合Rodinia超大陆古地理复原资料,推测扬子板块北东缘自新元古早期以来一直为接受大洋板块俯冲的活动大陆边缘.形成于新元古代中期的东海片麻状碱性花岗岩属A2型花岗岩,为弧后拉张背景下岩浆活动的产物,该类岩石的产出代表了Rodinia超大陆裂解事件在该地区的最初响应. 相似文献