The report marked with "*" before the serial number is a special invitation report (oral report) or a special topic convener report (posted report), and the report marked with "◎" before the serial number is a student report

第150专题  International Lithosphere Program: Progress and Opportunities
(召集人:Qin Wang,Zhonghai Li,Liang Zhao)
会议时间:10月21日　　会议地点:第37会议室,Room37(Fourth Floor,401)
主持人:QinWang，ZhonghaiLi
时间	序	报告题目	报告人
08:30-08:55	*1	The Tibetan Plateau as a passive wide-rift system	Irina M.Artemieva
08:55-09:10	2	Transient Acceleration and Termination of Japan Sea Opening Controlled by Oblique Subduction Induced Slab Window and Mantle Flow	Peigen Luo(骆沛根)
09:10-09:25	3	How do carbon and water from stagnant slabs thin the North China Craton?	Yiren Gou(苟乙人)
09:25-09:40	4	Thermal Consequences of Progressive Sediment Accretion in the Makran Subduction Zone	Matin Khaledzadeh
09:40-09:55	◎5	Quantitative estimation of leucosome volume in migmatized eclogite and implications for exhumation dynamics of mafic crust	Chao Yan(严超)
09:55-10:10	◎6	Dual Controls on Lithospheric Dripping: The Role of Mantle Flow and Orogen Scale	Qiuling Wang(汪秋菱)
10:10-10:20		BREAK
10:20-10:45	*7	How Many Plates? Scaling Laws Governing Planetary Plate Tessellation	Chunan Tang(唐春安)
10:45-11:00	8	Continental Lithospheric Growth beneath Southern Alaska: Insight from the Joint Full-waveform Inversion.	Mijian Xu(徐弥坚)
11:00-11:15	◎9	Earthquake Source Parameters and Tectonic Implications in Central Mongolia	Nomin-Erdene Erdenetsogt
11:15-11:30	◎10	3D Seismic Velocity Structure of the Eastern North China Craton-Korean Peninsula: New Constraints on SCB-NCP Collision Models East of the Tan-Lu Fault	Junjie Hao(郝俊洁)
11:30-11:55	*11	Continental Plateaux Uplift by Eclogitization, Underplating and Crustal Melting	Hans Thybo
11:55-12:00	12	Short Presentation of Posters, New Projects of ILP: Connecting Lithosphere with Surface Processes	Qin Wang(王勤)

第150专题  International Lithosphere Program: Progress and Opportunities
3-5分钟口头汇报（原张贴报告）
时间:10月21日
序	报告题目	报告人
*284	Formation of the Paleoproterozoic Fanjingshan collisional orogen and the Neoproterozoic Jiangnan accretionary orogen in the eastern Yangtze Caton	Qin Wang

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