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| 1 | 青藏高原地壳与上地幔成层速度结构与深部层间物质的运移轨迹显示文摘在印度洋板块与欧亚板块碰撞、挤压作用下,促使深部物质重新分异、调整和运移,并导致了地壳的短缩增厚,而且造成了高原的整体隆升和深部壳、幔物质的侧向流展。基于青藏高原腹地和周边地域地壳与上地幔的成层速度结构,特别是其特异层序的展布研究表明,青藏高原地壳巨厚,但岩石圈却相对较薄;地壳中于深20±5km处存在一低速层,层速度为5.7±0.1km/s,厚度为8±2km;上地幔软流圈顶部深度为110±10km;下地壳与上地幔盖层物质以地壳低速层为上滑移面,以岩石圈漂曳的上地幔软流圈顶面为下滑移面,在印度洋板块N-NNE向力源作用下在同步运移,即形成了青藏高原腹地和周边地域特异的大陆地球动力学环境。 | 滕吉文 阮小敏 张永谦 胡国泽 闫亚芬 | 2012 | 岩石学报2012，28，12： | 41 |
| 2 | 利用Rayleigh波相速度和群速度联合反演青藏高原东北缘S波速度结构显示文摘利用青藏高原东北缘地区固定和流动地震台网2007年8月到2012年1月期间记录的远震波形,运用小波变换频时分析方法分别测定了1216和653条周期从15到140s的台站间基阶Rayleigh相速度和群速度频散曲线.通过对上述频散进行反演,重构了青藏高原东北缘分辨率高达0.5°×0.5°的2-D相速度和群速度分布图.然后通过对所提取到的每个格网点Rayleigh波相速度和群速度频散进行联合反演,得到了研究区下方一维S波速度结构.最后通过线性插值,得到了青藏高原东北缘下方地壳上地幔三维S波结构.结果表明,印度板块向北俯冲已经达到班公—怒江缝合带附近;在柴达木盆地北部祁连山下面我们发现了亚洲板块,且其没有表现出明显的向南俯冲的迹象;在两大板块中间,我们观测到延伸到250km深度的低速异常,该低速异常可能是地幔物质底辟上涌现象造成的. | 余大新 李永华 吴庆举 潘佳铁 张风雪 何静 | 2014 | 地球物理学报2014，57，3： | 28 |
| 3 | 青藏高原东北缘地壳结构变化的地球动力学意义显示文摘由于印度板块和欧亚板块的碰撞作用,且扬子地块和鄂尔多斯地块的阻挡,位于青藏高原东北缘的甘东南地区成为地形变化极为剧烈的一个梯度带.该区域地壳发生了明显缩短,形成了复杂的地壳结构,因此,该地区地壳内部结构的探测对于青藏高原隆升机制的认识具有重要意义.本研究利用布设在该区39个固定宽频带台站远震接收函数,得到了该区域地壳底界面起伏形态以及波速比分布的详细结果.该结果表明,该区域地壳底界面存在着可达20km的起伏;接近青藏高原内部的研究区西部地壳较厚、波速比较大,该特性说明这一区域地壳中存在低速流变物质,是软地壳;位于鄂尔多斯和扬子地块的东边区域,地壳较薄、波速比较小,可能是硬地壳.在地形剧烈变化且位于软硬地壳之间的梯度带内,地壳厚度和波速比也呈现较为复杂分布,这可归结为长期复杂块体相互作用的结果.在历史上发生过海原巨大地震的局部区域,地壳起伏和波速比呈现较强烈的横向变化,这可能是该区域孕育巨大地震的一种深部结构条件. | 沈旭章 周元泽 张元生 刘旭宙 秦满忠 李翠芹 | 2013 | 地球物理学进展2013，28，5： | 20 |
| 4 | Characteristics of the crustal magnetic anomaly and regional tectonics in the Qinghai-Tibet Plateau and the adjacent areas显示文摘Study of the characteristics of the crustal magnetic anomaly in the Qinghai-Tibet Plateau and the adjacent areas helps better understand the lithospheric structure and evolution, as well as the regional geodynamic processes. Here we analyze the distribution laws of the crustal magnetic anomaly and its vertical gradient, the decay characteristics of the anomaly, the contributions from different wavelength bands to the anomaly, and the relationship between the anomaly and the crustal regional tectonics in the plateau and nearby, based on a new and higher degree geomagnetic model NGDC-EMM-720-V3 constructed from the surface, aeromagnetic, marine and satellite survey data. The results reveal that the positive and negative anomalies in the Qinghai-Tibet Plateau are weak, while those of the surrounding areas are strong. The boundary agrees well with the border of the plateau regional tectonics. The anomaly is nearly east-west in the central and western plateau, arc-shaped in the southwestern and eastern, and nearly north-south in the southeastern, consistent with the tectonic trends. There are strong negative anomaly foci in the east and west syntaxis, whereas no significant differences exist among the Cenozoic blocks in the plateau interior. No direct correspondence exists between the anomaly and the crustal depth. On the background of a weak magnetic anomaly in the plateau, relatively stronger short wavelength fields from the shallower crust are overlapped in the Lhasa, Qilian, Qaidam, and Sichuan-Yunnan rhombic blocks. A strong negative anomaly in the east-west direction is distributed along the Himalayas, mainly caused by the middle and long wavelength bands in the deep and central crust. The magnetic structural layers are stable in the Sichuan and Tarim basins. The anomalies at different altitudes over the southern plateau vary strongly, showing a drastic variation in the magnetic structure from the deep crust to the shallow crust. | KANG GuoFa GAO GuoMing BAI ChunHua SHAO Dan FENG LiLi | 2012 | Science China Earth Sciences2012，55，6： | 11 |
| 5 | 基于Love波相速度反演南北地震带地壳上地幔结构显示文摘收集了南北地震带区域地震台网中292个地震台站2008年1月至2011年3月期间的地震波形数据,由频时分析方法提取了Love波相速度频散曲线,经过反演得到了研究区内的Love波相速度分布.根据Love波纯路径频散,采用线性反演方法对0.25°×0.25°的网格点进行了一维S波速度结构反演,利用线性插值获取了南北地震带地区的三维S波速度结构.结果显示了松潘—甘孜地体和川滇菱形块体地区的下地壳具有明显的S波低速层分布,该异常分布特征支持解释青藏高原隆升及其地壳物质运移的下地壳流模型.在100至120km深度上,川滇菱形块体西北部呈现较强的S波高速异常,这可能是印度岩石圈板块沿喜马拉雅东构造结下插至该区域所致,该区域下地壳的低速软弱物质与上地幔的高速强硬物质形成了鲜明对比,暗示了地壳和上地幔可能具有不同的构造运动和变形方式,这为该区域的壳幔动力学解耦提供了条件. | 徐小明 丁志峰 叶庆东 吕苗苗 | 2015 | 地球物理学报2015，58，11： | 10 |
| 6 | Identification of an Early–Middle Jurassic oxidized magmatic belt,south Gangdese,Tibet,and geological implications显示文摘The south Gangdese region is the site of subduction of the Neo-Tethys and subsequent continental collision. Compared with widespread Cretaceous and Cenozoic magmatism, Early–Middle Jurassic magmatic rocks and related deposits are rarely reported. Our work identified a >200 km long felsic rock belt associated with Cu mineralization in the south Gangdese region. We report here zircon U–Pb ages, zircon Ce^(4+)/Ce^(3+)values, and mineral assemblages of two Cu mineralized intrusions within the belt. A hornblende granite and a diorite porphyry were emplaced at 177.3 Ma and 166.3 Ma, respectively.Geological occurrence and magmatic hematite–magnetite–chalcopyrite intergrowths suggest that Cu mineralization formed coeval with Jurassic intrusions. Mineralized intrusions have high zircon Ce^(4+)/Ce^(3+)and EuN/Eu?N ratios, and hematite–magnetite intergrowths, suggesting their parent magmas were highly oxidized. Hornblende is common and primary fluid inclusions are found in titanite and apatite,indicating their parent magmas were water-saturated and exsolved volatile phases at early stage of magmatic evolution. Those magma characters contribute to the formation of porphyry Cu deposits. Given that majority subduction-related porphyry Cu systems have been eroded following uplift and denudation, the well-preserved Early–Middle Jurassic Cu mineralized igneous rocks in south Gangdese are favorable prospecting targets for subduction-related porphyry Cu deposits. | Yinqiao Zou Xilian Chen Wenting Huang Jian Zhang Huaying Liang Jifeng xu Ling Chen | 2017 | Science Bulletin2017，62，12： | 7 |
| 7 | Application study of a correction method for a spacecraft thermal model with a Monte-Carlo hybrid algorithm显示文摘The correction of a thermal model for a thermally controlled satellite in ground test conditions is studied using a Monte Carlo hybrid algorithm.First,the global and local parameters are summarized according to sensitivity analyses on uncertain parameters,and then the model correction is treated as a parameter optimization problem to be solved with a hybrid algorithm.Finally,the correction of the thermal model is completed using a layered correction method.The sensitivity analysis showed that the effective emissivities across the multi-layer insulation (MLI) and the emissivities of the thermal control coating are global parameters,while the contact heat transfer coefficients are local parameters.After correction,the deviations between the calculated and test values were all within ± 3 ℃.The final results prove that the method in this study is superior to traditional methods and satisfies the requirements for thermal model correction. | CHENG WenLong LIU Na LI Zhi ZHONG Qi WANG AiMing ZHANG ZhiMin HE ZongBo | 2011 | Chinese Science Bulletin2011，56，13： | 2 |
| 8 | Seismic P-wave tomography in eastern Tibet: Formation of the rifts显示文摘为更好学习在裂缝和深结构之间的关系,在东方西藏下面的详细 P 波浪速度结构从由 51 个便携式的车站记录的 169 个 teleseismic 事件用 4767 到达时间被建模。在通过模型的水平片,一个突出的低速度的异例从表面在裂缝下面被检测到 250 km 的深度;这在垂直的片延长到 400 km 的深度。这个低速度的异例作为上面的披风 upwelling 被解释。做的观察为纵贯的 trending 裂缝的形成提供地震证据。低速度的异例的东方,一个清楚的高速度的异例在 40 和 200 km 的深度之间被发现。由于它的浅深度,我们建议它从古老的大陆人闭合而非印度板由材料组成。从 250 ~ 400 km 的深度,一个高速度的异例出现到 Jiali 差错的南方。这个异例可以对应于在喜玛拉雅的块下面从表面分开了的印度板的北边。我们建议印度板 underthrusts 不在东方西藏比 Jiali 差错推进。 | ZHANG Heng ZHAO JunMeng XU Qiang | 2011 | Chinese Science Bulletin2011，56，23： | 2 |
| 9 | Characteristics of the crustal and mantle structures across Lhasa terrane显示文摘The Himalayan-Tibetan orogen is the youngest and arguably most spectacular of all the continent-continent collisional belts on the Earth. There are not only north-south extrusions but also east-west extensions in the Tibetan Plateau. All these phenomena are the results of the Indian plate subducting into the Eurasia plate about 70 Ma | Hongwei Zheng Rizheng He Xuan Guo | 2009 | Earthquake Science2009，22，4： | 0 |
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