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宁杰远
电话: 62765852
类别: 科研

标题 6月15日(星期五)下午3:00优赛科技北大地球物理学术报告会   发布时间 2018年6月13日15时23分 星期三
Title:GNSS Atmospheric Seismology: Observations and Modelling
Presenter: Senior Research Scientist  Shuanggen JIN
Institution: Shanghai Astronomical Observatory
Time: 20180615-15:00:00
Location: Room 2829, No. 2 Science Building.

Abstract
Earthquakes often occur and result in civilian casualties and huge Damages. However, it is still a challenge to know the detail and nature of earthquakes as well as predict earthquakes up to now due to lack of dense near-field observations and traditional techniques limitations. Nowadays, the atmospheric parameters and ionospheric total electron content (TEC) can be obtained from global navigation satellite system (GNSS) and other remote sensing data, which can be used to investigate the seismo-atmospheric disturbances and may provide insights on the earthquake. In this talk, seismo-atmospheric disturbances from GNSS and other remote sensing data are presented and reviewed, including observations, theory, methods, recent results and characteristics. The ionospheric perturbations are generated close to the epicenter as acoustic-gravity waves and the atmosphere/ionosphere acoustic and gravity waves by surface Rayleigh waves and tsunamis respectively. These waves are induced by solid-Earth/ocean and atmosphere coupling at the ground or ocean interface with the atmosphere propagating upward until the ionosphere create strong perturbation in plasma density and plasma velocity.

Keywords: Seismo-atmospheric disturbances, GNSS, Remote Sensing

Reference: Jin, S.G., G. Occhipinti, and R. Jin (2015), GNSS ionospheric seismology: Recent observation evidences and characteristics, Earth-Sci. Rev., 147, 54-64, doi: 10.1016/j.earscirev.2015.05.003.

报告人简介:
金双根,1974年生,博士,俄罗斯自然科学院外籍院士,国际大地测量协会(IAG)会士,中科院"百人计划",中科院上海天文台研究员,南京信息工程大学遥感与测绘工程学院院长和教授。长期从事卫星导航、大地测量、卫星遥感、全球变化和空间行星探测,发表SCI论文近150余篇,EI检索100余篇,出版著作和教科书8部,被Nature等引用3400余篇次,H指数大于36,获国家发明专利和软件著作权8项,国际会议特邀报告100余次。担任国际IUGG委员会主席,全球华人导航定位协会主席(2016),国际大地测量(IAG)委员会副主席,国际期刊IJG主编,IEEE TGRS、JN和ASR副主编,RS、JG、PSS和GPS Solut.编委等,以及获省部级科技进步一等奖1项和二等奖4项等。

宁杰远
电话: 62765852
类别: 科研

标题 6月8日(星期五)下午3:00优赛科技北大地球物理学术报告会  发布时间 2018年6月4日9时9分 星期一
报告题目:数据导向型模型在俯冲动力学和大陆岩石圈演化中的应用——以南美为例
报告人:胡佳顺 博士
报告人单位:伊利诺伊大学
报告时间:20180608-15:00:00
报告地点:理科二号楼2829

报告摘要:南美洲具有复杂的地质地貌现象。其西海岸是世界上最长的俯冲带,包括多个平俯冲板片,而东海岸则有着巨大的巴西高原。地震波速的研究揭示出南美洲上地幔的各向异性非常复杂,但具有一定的规律性。这些现象及其动力学成因仍然是一个未解之谜。我们利用数据导向型模型来定量地研究南美洲这些复杂的地质地球物理现象。基于这个模型,我们发现平俯冲板片的形成与海山和大洋高原的俯冲有关,而俯冲板片引起的地幔对流能够同时解释南美洲的SKS和面波各项异性。同时,结合地质观测、动力地形、重力异常以及各向异性,我们发现克拉通具有分层结构,下层较重的岩石圈拆沉会导致地形隆起。这可以解释巴西高原和非洲南部的地形异常,同时对克拉通演化以及稳定性的研究具有重要意义。

参考文献:
[1]Hu J, Liu L, Faccenda M, et al. Modification of the Western Gondwana craton by plume–lithosphere interaction[J]. Nature Geoscience, 2018.
[2] Hu J, Liu L, Hermosillo A, et al. Simulation of late Cenozoic South American flat-slab subduction using geodynamic models with data assimilation[J]. Earth & Planetary Science Letters, 2016, 438:1-13.

报告人简介:胡佳顺2013年获北京大学地球物理学学士学位,2018年获伊利诺伊大学地质学博士学位。胡佳顺博士的研究主要集中于俯冲带、岩石圈演化、地震波各向异性等地球动力学课题。其先后在NGeo, EPSL等期刊发表多篇重要学术论文。
宁杰远
电话: 62765852
类别: 科研

标题 6月1日(星期五)下午3:00优赛科技北大地球物理学术报告会  发布时间 2018年5月29日9时8分 星期二
报告题目:科研档案管理规范与科技文件材料收集及归档案卷整理
报告人:马青 高级工程师
报告人单位:中国地震局第一监测中心
报告时间:20180601-15:00:00
报告地点:理科二号楼2829

报告摘要:
  科研档案是科学研究进展过程的真实记录,如何依法依规做好科技文件材料收集及归档案卷整理工作往往容易被忽视。本报告依据科研档案管理规范与要求,结合科研项目由申报、批复到科研工作实施至结题验收过程,重点讲述怎样做好科技文件材料收集、如何进行归档案卷整理形成科研档案和档案管理中应注意的一些问题。

科研档案管理规章:
  1. 科学技术研究课题档案管理规范,DA/T 2-1992
  2. 科学技术档案案卷构成的一般要求,GB/T 11822—2008
  3. 纸质归档文件装订规范,DA/T 69-2018(待实施)

报告人简介:
  马青,高级工程师,本科毕业于武汉大学信息工程学院(后学历)。1979年参加工作在中国地震局第一监测中心(简称一测中心),曾从事地震台站观测与基础科学研究辅助工作,合作发表论文20余篇。2006年起正式从事科技档案管理工作至今,先后参加或主持完成了中国地震局系统单位和一测中心承担的国家重大项目的科技档案建立工作;近3年,受中国地震局办公室委托,主持完成了部分由中国地震局承担的国家重大建设项目和科研项目的档案专项验收工作。

宁杰远
电话: 62765852
类别: 科研

标题 5月28日上午10:30地球物理学术报告会  发布时间 2018年5月28日0时25分 星期一
Recent Advances in Large-N, Large-T and Machine Learning Seismology

Dr. Zefeng Li(California Institute of Technology)

    Long-term seismic data accumulation (known as Large-T) and ultra-dense seismic instrumentation (known as Large-N) are major momentums for the rapid growth in the quantity of seismic data. Long-term accumulated seismic data provide indispensable resources for seismological research. In particular, permanent high-quality seismic networks (e.g., SoCal network, Hi-net) that have been operated for decades are regularly used in seismological research, which greatly advance our understanding of the earthquake phenomena and the Earth’s structures. On the other hand, temporary seismic networks, which commonly operate from weeks to years, have become increasingly dense in order to achieve high-resolution imaging of the Earth. Among them nodal arrays and distributed acoustic sensing (DAS) are outstanding examples. The unprecedented big volume of seismic data pose great challenges for processing and analysis techniques in modern seismology. Correspondingly, nowadays machine learning has provided a large collection of tools to handle voluminous data. In this talk, I will briefly introduce the emerging global race in big seismic data and machine learning seismology, and make a holistic presentation of our recent efforts in 1) Large-N microseismic detection using both nodal arrays and DAS data; 2) machine learning applications to Large-T with emphasis on earthquake early warning.

时间: 2018年5月28日星期一10:30AM
地点: 北京大学理科2号楼2807S

欢迎各位参加!
宁杰远
电话: 62765852
类别: 科研

标题 5月25日(星期五)下午4:00优赛科技北大地球物理学术报告会  发布时间 2018年5月22日20时45分 星期二
报告题目:大地电磁深部探测:以华南地块为例
报告人:胡祥云 教授
报告人单位:中国地质大学(武汉)地球物理与空间信息学院
报告时间:20180525-16:00:00
报告地点:理科二号楼2829

报告摘要:采用天然电磁场的大地电磁探测方法是研究地球深部结构的重要手段之一。利用大地电磁数据获取的岩石圈电性结构能够指示地球物质结构、组成以及赋存状态,一方面可以反映构造特征,约束岩石圈热状态和流变性,揭示大陆的形成、演化及深部动力学机制;另一方面,可以为油气及矿产资源的远景评估和勘探提供重要基础支撑。在以往各国实施的岩石圈深部结构探测计划中,大地电磁探测都是重要组成部分。国内外学者利用大地电磁法在岩石圈壳幔结构、深部物质运移、壳幔中流体物质的分布、大陆强震孕育环境等重要地球科学问题的研究中取得了许多显著成果。华南地块是欧亚板块东南缘地壳生长和核-幔质量传输强烈的构造带,我国花岗岩体分布最为广泛的地区,具有罕见的世界级多金属成矿省,是研究大陆动力学演化与成矿作用的理想基地。利用大地电磁数据可以构建华南地区岩石圈电性结构模型,研究岩石圈温度、压力、流变性等物理状态,为深部流体的运移、大规模构造岩浆运动与成矿作用提供重要启示。

参考文献:Meqbel N M, Egbert G D, Wannamaker P E, et al. Deep electrical resistivity structure of the northwestern U.S. derived from 3-D inversion of USArray magnetotelluric data[J]. Earth & Planetary Science Letters, 2014, 402(6):290-304.

报告人简介:胡祥云,教授,博士生导师。于长春地质学院获应用地球物理学士和硕士学位,中国地质大学获矿产普查与勘探博士学位。1994 年进入中国地质大学(武汉)从事地球物理教学与科研工作至今,现任地球物理与空间信息学院院长。长期从事深地电磁探测与深部资源勘探应用研究。基于MPI的大地电磁三维并行算法、重磁电三维顺序联合反演算法、基于概率密度的地球物理算法和基于盲信号的深部矿产弱异常提取及精细定位等方法研究,提高了复杂、深部矿产的预测精度和计算速度。现为中国地球物理学会理事、电磁专业委员会常务委员。发表各类学术论文100余篇。
宁杰远
电话: 62765852
类别: 科研

标题 5月17日(星期四)下午4:00优赛科技北大地球物理学术报告会  发布时间 2018年5月16日9时22分 星期三
Title:Remote triggering of earthquakes as a potential stress-meter: the case of the 2016 M7.3 Kumamoto (Kyushu) mainshock
Presenter: Associate Professor Bogdan Enescu
Institution: Department of Geophysics, Kyoto University
Time: 20180517-16:00:00
Location: Room 2829, No. 2 Science Building.

Introduction. Distant earthquake triggering is relatively scarce in Japan (Harrington and Brodsky, 2006), except for the remote seismicity activated following the 2011 M9.0 Tohoku-oki earthquake (e.g., Opris et al., 2018). Here we report on a widespread remote triggering of small events after the 2016 M7.3 Kumamoto earthquake and discuss implications on the stress-state at inland active faults and volcanoes throughout Japan
.
Data and methods. We have processed waveform data recorded at high-sensitivity Hi-net and broadband F-net stations (NIED) allover Japan. The waveforms were scrutinized in high and low frequency ranges to detect remote events occurred during the passage of mainshock surface waves. Dynamic stresses were estimated using the approach of Peng et al. (2009).

Results. The remotely activated seismicity correlates well with the passage of the surface waves from the Kumamoto earthquake. Triggering was observed at volcanoes in Hokkaido (at an epicentral distance of ~1630 km), Tohoku, Chubu, Izu Peninsula, and southern part of Kyushu, as well as active fault areas in Wakayama, Tottori and Noto Peninsula. The remote dynamic stresses are significant, ranging from several to tens of kPa. Since most of the remotely triggered events occurred at volcanoes, we suggest that excitation of fluids is the main activation mechanism. The strong shaking, due to a clear directivity effect, may explain the observed spatial distribution of triggered earthquakes as well as their long-range extent.

Conclusions. It is very important to understand why such widespread remote activation has not been observed before in Japan, at similar dynamic stress levels. We found that many of the regions activated this time have been also activated after the 2011 Tohoku-oki earthquake. We hypothesize that mechanical weakening of a pressurized crust, due to the 2011 megathrust, might be responsible for an increased trigger-ability. The earthquake triggering at some active crustal faults might be related to the regional levels of tectonic stress. All these observations suggest that remote triggering could be used as a stress-meter at volcanoes and active faults and thus might have applications in earthquake hazard assessment and forecasting.

References
Opris, A., Enescu, B., Yagi, Y., and J. Zhuang, Triggering and decay characteristics of dynamically activated seismicity in Southwest Japan, Geophys. J. Int., 212, 2, 1010-1021, doi: 10.1093/gji/ggx456, 2018.
Enescu, B., Shimojo, K., Opris, A., and Y. Yagi, Remote triggering of seismicity at Japanese volcanoes following the 2016 M7.3 Kumamoto earthquake, Earth, Planets and Space, 68:165, doi: 10.1186/s40623-016-0539-5, 2016.

Homepage:www-seis.kugi.kyoto-u.ac.jp/~benescu/e-index.html
宁杰远
电话: 62765852
类别: 科研

标题 5月18日(星期五)下午3:00优赛科技北大地球物理学术报告会  发布时间 2018年5月15日8时42分 星期二
报告题目:六盘山深部地壳结构及其对高原扩展的指示意义
报告人:田小波 研究员
报告人单位:中国科学院地质与地球物理研究所
报告时间:20180518-15:00:00
报告地点:理科二号楼2829

报告摘要:为研究高原与周缘克拉通的接触关系,2016年实施了跨六盘山的东西向剖面短周期密集台阵天然地震观测,利用接收函数构建地壳结构,结果显示了异常的变化特征,可能对克拉通地壳向高原地壳转变具有重要指示作用。

参考文献:Zhen Liu, Xiaobo Tian*, Rui Gao, Gaochun Wang, Zhenbo Wu, Beibei Zhou, Ping Tan, Shitan Nie, Guiping Yu, Gaohua Zhu, Xiao Xu, 2017. New images of the crustal structure beneath eastern Tibet from a high-density seismic array. Earth and Planetary Science Letters, 480, 33-41, doi: 10.1016/j.epsl.2017.09.048.

报告人简介:报告人主要从事青藏高原及其周缘壳幔结构地震学探测和动力学研究,致力于通过深部结构研究和约束浅表构造活动、演化的深部过程;第一作者、通讯作者发表SCI论文二十余篇,主持过多项自然科学基金项目、公益性行业专项课题、科学院先导专项B课题等;所在研究团队在青藏高原南北向裂谷、高原中部共轭走滑断层形成、高原周缘扩展的深部结构和动力学过程的研究取得了系列新成果;近年来,积极组织和实施短周期密集台阵探测壳幔结构,快速获取高分辨壳幔结构图像,取得良好效果,其中若尔盖-九寨沟剖面结果2017年在EPSL结果;近期在近三年来累计剖面长度约两千多公里。

报告人主页:http://sourcedb.igg.cas.cn/cn/zjrck/200907/t20090713_2065436.html

宁杰远
电话: 62765852
类别: 科研

标题 5月11日(星期五)下午3:00优赛科技北大地球物理学术报告会  发布时间 2018年5月6日19时15分 星期日
Title:Origin of the Moon: An Attempt to Solve the Isotopic Crisis
Presenter: Prof. Shun-ichiro Karato
Institution: Department of Geology & Geophysics, Yale University
Time: 20180511-15:00:00
Location: Room 2829, No. 2 Science Building.

Abstract: A giant impact model has been a standard model for the formation of the Moon. However, most of models showed that the Moon is mostly formed from the impactor and explaining the close similarity in the isotopic compositions is difficult. Many modified models have been proposed where different mechanical aspects of collision were considered. However, these models have difficulties in explaining the angular momentum, and successful models can be found only in a very small parameter space. Here we propose a new model where the giant impact by a solid impactor occurred to the proto-Earth that was covered with a magma ocean. Due to the large differences in the shock heating between silicate melts and solid silicates (rocks) shown by a new theory of equation of state of silicate melts, a substantial fraction of the ejected material is from the magma ocean even with a highly oblique collision. This model provides a natural explanation of the isotopic similarities between the Moon and Earth with the angular momentum constraint being satisfied

Homepage:https://people.earth.yale.edu/profile/shun-ichiro-karato/about

CV:SHUN-ICHIRO KARATO

(a) Professional preparation:
University of Tokyo, Tokyo (Japan), Geophysics, BSc., 1972
University of Tokyo, Tokyo (Japan), Geophysics, MSc., 1974
University of Tokyo, Tokyo (Japan), Geophysics, Ph.D., 1977

(b) Appointments:
2001-present Professor, Department of Geology & Geophysics, Yale University
1992- 2001 Professor, Department of Geology & Geophysics, University of Minnesota
1989-1992 Associate Professor, University of Minnesota
1981-1984 Research Fellow, Australian National University
1977-1989 Assistant Professor, Ocean Research Institute, University of Tokyo

(c) Awards/honors

Alexander von Humboldt Prize 1995
Vening Meinesz lecture (Utrecht University) 1998
Japan Academy Prize 1999
Fellow of American Geophysical Union 2000
Birch lecture (AGU) 2004
Vening Meinesz medal (VMSG) 2006
Fellow of Mineralogical Society of America 2011
Augustus Love medal (EGU) 2014
Fellow of Japan Geoscience Union 2014
Inge Lehmann medal (AGU) 2016

(d) Publications

Karato, S., Paterson, M.S. and Fitz Gerald, J.D., 1986.  Rheology of synthetic olivine aggregates:  influence of grain size and water, J. Geophys. Res., 91: 8151-8176.
Karato, S. 1990.  The role of hydrogen in the electrical conductivity of the upper mantle, Nature, 347: 272-273.
Karato, S., 1992. On the Lehmann discontinuity, Geophys. Res Lett., 19: 2255-2258.
Karato, S. and P.Wu, 1993. Rheology of the upper mantle: A synthesis, Science. 260: 771-778.
Karato, S., 1993. Importance of anelasticity in the interpretation of seismic tomography, Geophys. Res. Lett., 20: 1623-1626
Zhang, S. and S. Karato, 1995. Lattice preferred orientation in olivine due to shear deformation, Nature, 375: 774-777.
Karato, S. and Jung, H., 1998. Water, partial melting and the origin of the seismic low velocity and high attenuation zone in the upper mantle, Earth Planet Sci. Lett., 157: 193-207.
Jung, H. and Karato, S., 2001. Water-induced fabric transitions in olivine, Science, 293: 1460-1463.
Bercovici, D. and Karato, S., 2003. Whole-mantle convection and the transition-zone water filter, Nature, 438: 39-44.
Huang, X., Xu, Y. and Karato, S., 2005. Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite, Nature, 434: 746-749.
Wang, D., Mookherjee, M., Xu, Y. and Karato, S., 2006. The effect of hydrogen on the electrical conductivity in olivine, Nature, 443: 977-980.
Karato, S., 2008. Deformation of Earth Materials: Introduction to the Rheology of Solid Earth, Cambridge University Press, Cambridge, pp. 463.
Karato, S., 2011. Water distribution across the mantle transition zone and its implications for the global material circulation, Earth Planet. Sci. Lett., 301: 413-423
Karato, S. 2012. On the origin of the asthenosphere, Earth, Planet. Sci. Lett., 321/322: 95-103.
Otsuka, K. and Karato, S., 2012. Deep penetration of molten iron into the mantle caused by the morphological instability, Nature, 492, 243-236.
Dai, L. and Karato, S., 2014. High and highly anisotropic electrical conductivity of the asthenosphere due to hydrogen diffusion in olivine, Earth Planet. Sci. Lett., 408: 79-86.
Karato, S., Olugboji, T., and Park, J., 2015. Mechanisms and geologic significance of the mid-lithosphere discontinuity in the continent, Nature Geoscience, 8: 509-514.
Girard, J., Amulele, G., Farla, R., Mohiuddin, A. and Karato, S., 2016. Shear deformation of bridgmanite + magnesiowüstite aggregates under the lower mantle conditions, Science, 251: 144-147.


(e) Synergetic activities
The PI was on the geophysics panel of NSF (2001-2004)
The PI was on the executive committee (vice chair) of COMPRES (2002-2005)
The PI is on the advisory board of IUGG (2011-2015)
The PI is on the advisory board of JpGU (2013-)
The PI is a member of Geodynamics section of EGU (2014-)


宁杰远
电话: 62765852
类别: 科研

标题 地球科学大数据与人工智能大型学术研讨会  发布时间 2018年5月3日15时10分 星期四
北大校庆系列活动暨优赛科技北大地球物理系列报告之
地球科学大数据与人工智能大型学术研讨会
(会议通知)

北京,2018年5月7-9日

一、会议召开背景:
    人工智能已在很多领域发挥重要作用,而且起着越来越重要的作用。为了加速人工智能的有效应用,让人工智能理论和方法与地球科学实际问题对接,促进地球科学发展,在北大120周年校庆之际,北京大学等单位特别发起了“地球科学大数据与人工智能大型学术研讨会”。特别邀请了国际人工智能协会主席杨强教授,以及进行过尝试性人工智能研究或富有行业经验的地球科学专家与会,介绍各自的研究成果,并进行现场互动,旨在通过深入讨论加深对于如何正确地运用人工智能方法解决地球科学问题的认识,推动人工智能应用及地球科学快速发展。

二、会议发起单位
    北京大学地球与空间科学学院
    北京大学信息科学技术学院
    中国科学院油气资源研究重点实验室
    北京地球物理学会
    北京优赛科技有限公司    
    国际勘探地球物理学会(SEG)
    沙特阿美先进技术研究中心
    通联数据工程公司
    南方科技大学
    同济大学

三、会议组织机构

1、学术指导委员会:张立飞、黄清华、赵里、高锐、郑永飞

2、专业委员会:
    宁杰远、蒋云(北京大学)
    李幼铭、王彦飞(中国科学院地质与地球物理研究所)
    俞度立(北京化工大学)
    骆  毅(沙特阿美先进技术研究中心)
    房立华(中国地震局地球物理研究所)
    杨顶辉(清华大学)
    刘  韬(中石化研究院)
    马坚伟(哈尔滨工业大学)
    耿建华(同济大学)

3、会议联系人:
    孟晓燕:m254775788@sina.com,18201102023;
    温景充:1400012411@pku.edu.cn,18811782928;
    鲍铁钊:yu_fei_btz@163.com,18811465204。

四、会议时间和地点

    会议时间:2018年5月7-9日。
    会议地点:北京大学中关新园一号楼二楼学术报告厅
    报到时间:2018年5月7日14:00-18:30;报到地点:北大中关新园一号楼大厅
    疏散时间:2018年5月9日

五、2018年5月8日会议日程安排

报告时间 报告人 报告题目
8:30-10:30 杨  强 普惠的人工智能
10:30-11:00 茶  歇
11:00-12:00 和杨强教授现场互动:“让人工智能有效惠及地球科学”
12:00-13:30 午  餐(北京大学农园三楼)
13:30-13:55 黄  磊 地质体分类的深度学习研究
13:55-14:20 马坚伟 深度学习地震数据去噪和反演
14:20-14:45 杨午阳 塔里木盆地地震勘探资料中突出的噪音类型及分析
14:45-15:10 陆文凯 智能地震初至拾取:初步结果
15:10-15:30 茶  歇
15:30-15:55 林年添 地震油气储层的卷积神经网络学习与预测
15:55-16:20 曹俊兴 基于地震数据深度学习的天然气储层预测
16:20-16:45 刘忠宝 智能分类方法研究
16:45-17:10 郑晓东 数据及模型驱动下的智能地震勘探技术

六、其它事项:

1.免注册费;
2.食宿及交通费自理;
3.会议提供茶歇及5月8日的午餐;
4.可开具会议证明。

                                               北京大学地球与空间科学学院
                                               北京大学信息科学技术学院
                                               2018年5月3日

张献兵
电话:
类别: 科研

标题 Invitation of The Second Young Geophysicists Forum of Peking University  发布时间 2018年5月1日21时36分 星期二
The past decade has seen a global advancement of geophysical research. New observations, theories and computational technologies have generated unprecedented opportunities for the development of geophysics. The Institute of Theoretical and Applied Geophysics (ITAG) of Peking University is the premier institution in geophysical education and research in China, and the goal of ITAG is to attract promising researchers to conduct frontier research by promoting an open and free academic environment.
The Second Young Geophysicists Forum of Peking University will be held July 24-27, 2018, in Beijing, China. The purpose of this forum is to provide a platform for young geophysicists to share their research experiences and enhance collaboration. This year, the forum will coincide with the 120th anniversary of Peking University, and we sincerely invite outstanding young geophysicists of all nationalities to join us. Funding opportunities are available, including full travel support for selected oversea participants.
Eligibility of Participation
Recent Ph.D. (preferably within 5 years) in Geophysics or a related discipline or planning to receive a doctor degree in one year.
A competitive track record of independent research.
Support
Part of selected applicants could receive a full coverage of traveling and living expenses related to the forum.
Time-line
May 20, 2018: deadline of application for travel support.
May 30, 2018: decision on travel support.
June 30, 2018: deadline of abstract submission.
July 24-27, 2018: the Forum.

Visit http://geophy.pku.edu.cn/2018/forum for updates.
Please send CV and research statement to the following email address
Xianbing Zhang (xbzhang@pku.edu.cn)

go to “youth forum”

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