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| 1 | Recent Developments of Earthquake Early Warning in California,USA显示文摘In this paper we outline the science,engineering,and societal considerations of the prototype Earthquake Early Warning System( EEWS) in California and detail the development and testing of methodologies in the last 10 years in America. Also,we give a brief introduction of Earthquake Early Warning( EEW) in China,and based on the summary of EEW in California we make an analysis of the perspectives,misconceptions,and challenges that China may have. | Wang Honglei Walter D.Mooney | 2014 | Earthquake Research in China2014，28，3： | 0 |
| 2 | Identification of the Early Jurassic mylonitic granitic pluton and tectonic implications in Namling area,southern Tibet显示文摘A number of studies revealed that the Gangdese magmatic belt of southern Tibet was closely related to the northward subduction of the Neo-Tethys oceanic lithosphere and Indo-Asian collision.However,pre-Cretaceous magmatism is still poorly constrained in the Gangdese magmatic belt,southern Tibet.Here,we conducted systematically geochronology and geochemistry studies on a newly-identified granitic pluton in the middle Gangdese magmatic belt(Namling area),southern Tibet.Zircon SHRIMPⅡU-Pb dating for one representative sample gives a weighted age of 184.2±1.8 Ma(MSWD=±1.11),corresponding to emplacement and crystallization age of the granitic pluton in the Early Jurassic(Pliensbachian).High SiO2(68.9-72.1 wt.%)contents and intermediate Mg#values(35-38)together suggest that the newly-identified granitic pluton was probably formed by partial melting of crustal material with minor injection of mantle-derived magma,precluding an origin from melting of metasedimentary rocks that are characterized by low Mg#and high zirconδ^18O values(>8‰).Geochemically,the newly-identified granitic pluton belongs to typical I-type granitic affinity,whereas this is inconsistent with aluminium saturation index(ASI=A/CNK ratios)and geochemical signatures.This suggests that zircon oxygen isotopes(4.30‰-5.28‰)and mineral features(lacking Al-rich minerals)are reliable indicators for discriminating granitic origin.Significantly depleted whole-rock Sr-Nd-Hf isotopic compositions and zirconεHf(t)values indicate that the granitic pluton was derived from partial melting of depleted arc-type lavas.In addition,the granitic pluton shows zirconδ^18O values ranging from 4.30‰to 5.28‰(with a mean value of 4.77‰)that are consistent with mantle-derived zircon values(5.3‰±0.6‰)within the uncertainties,indicating that the granitic pluton might have experienced weak short-living high-temperature hydrous fluid-rock interaction.Combined with the Sr-Nd-Hf-O isotopes and geochemical signatures,we propose that the newly-identified granitic pluton was originated from partial melting of depleted mafic lower crust,and experienced only negligible wall-rock contamination during ascent.Integrated with published data,we also propose that the initial subduction of the Neo-Tethys oceanic lithosphere occurred no later than the Pliensbachian of the Early Jurassic. | Yuanku Meng Walter D.Mooney Runlong Fan Jinqing Liu Youqing Wei | 2021 | Geoscience Frontiers2021，12，1： | 0 |
| 3 | 南美洲及周边洋盆的地壳和地幔顶部结构显示文摘给出了南美洲及周边洋盆一套新的地震波结构等值线图。这些图使用了新数据,因而更好地约束了地壳厚度、全地壳P波和S波的平均速度以及地幔顶部的地震波速度(Pn和Sn)。我们发现:(1)南美洲地壳厚度的加权平均值为38.17km(标准差为±8.7km),这比全球陆壳平均值39.2km要薄约1km;(2)南美洲全地壳P波速度的直方图呈双峰形态,其低峰值发生在缺失下地壳高速层(6.9-7.3km)的区域;(3)结晶地壳的P波平均速度(Pcc)为6.47km/s(标准差为±0.25km/s),这与全球平均值6.45km/s基本相同;(4)南美洲下方的Pn平均速度为8.00km/s(标准差为±0.23km/s),略低于全球平均值8.07km/s;(5)横贯智利北部与阿根廷东北部的地壳内存在一个P波和S波低速异常带,地理上正对应于纳斯卡板块浅俯冲部分[Isacks等在1968年首次提出的南美大草原(Pampean)平缓板块],同时也是一地壳拉张区域;(6)巴西克拉通的厚地壳一直延伸到委内瑞拉和哥伦比亚;(7)亚马逊盆地以及沿巴西克拉通西部边缘地壳可能由于拉伸作用而变薄;(8)东太平洋海床之下的地壳P波平均波速要大于其在西大西洋海床的数值,这可能源于较古老的大西洋海床覆盖了更厚的沉积层。 | Gary S.Chulick Shane Detweiler Walter D.Mooney 薛彬 刘伟 张瑞青 | 2015 | 世界地震译丛2015，46，4： | 0 |
| 4 | 西北太平洋俯冲带大地幔楔及地幔过渡带各向异性证据和特征显示文摘地震层析成像研究清晰给出了地球深部俯冲板片的大尺度形态,但与俯冲过程相关的地幔流动特征仍不明确.在俯冲地幔楔系统中,前人观测到了与海沟平行和垂直的快波偏振方向.本文研究了西北太平洋俯冲板片在地幔过渡带中停滞形成的'大地幔楔'中的各向异性特征.对具有长期稳定观测数据的MDJ台站SKS震相和区域深源地震的直达S波震相进行了详细的剪切波分裂研究.采用多波形同时反演方法在保证数据后方位角覆盖范围的基础上得到了更加精确的SKS震相各向异性结果.剪切波分裂参数具有明显的频率依赖性和随初始极化方向变化的特征,表明台站下方存在多个可能的各向异性源区.对不同频段各向异性观测结果的双层各向异性模型拟合表明,上层各向异性参数为φ=32°±12°,δt=1.4±0.4 s,表现出受郯庐断裂带影响的岩石圈中'固化'各向异性特征;下层各向异性参数为φ=-71°±6°,δt=2.4±0.4 s,与海沟近乎垂直.下层较大的各向异性延时表明研究区域的地幔楔和地幔过渡带中存在明显各向异性,推测是由地幔中软流圈流动引起的橄榄石晶格优势取向和停滞的西北太平洋板片引起的地幔水平流动产生的瓦兹利石晶格优势取向共同作用所导致. | 郭广瑞 李娟 陈思丹 Walter D.Mooney | 2021 | 地球物理学报2021，64，2： | 0 |
| 5 | Walter D.Mooney:期待SinoProbe伟大旅程的延续显示文摘SinoProbe科学项目拥有宏伟的蓝图。它研究地球的地质演化,探索珍贵自然资源的起源,它对地表无法接触到的地球深部结构进行探索,而这一切将会改变人类对其所居住的世界的理解。SinoProbe就像是一架瞄准地球内部的巨大望远镜,而不是高高悬在天空。SinoProbe的科学基础来源于旱先的国际地球科学项目,尤其是在欧盟、英国、加拿大、美国和澳大利亚开展的项目。而其中,加拿大和中国两个国家拥有很多的相似之处,比如都有丰富的自然资源。 | Walter D.Mooney 姜天海 | 2014 | 科学新闻2014，0，10： | 0 |
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