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会议指南 - 中国学术会议在线

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专题 8 深部地球–从地壳到地核<br />

Topic 8 Deep Earth- From Crust to Core<br />

2009.10.26 上午 08:30-11:45<br />

召 集 人 时 间 发 言 人 报 告 题 目<br />

刘 曦<br />

Jacques<br />

Charvet<br />

08:30-08:45 Lidong Dai* Grain boundary conductivities of peridotite at high temperature and high pressure<br />

08:45-09:00<br />

09:00-09:15<br />

09:15-09:30<br />

09:30-09:45<br />

Afroz Ahmad Shah<br />

Decoding the regional ~1700 Ma deformational history from the rocks of Big<br />

Thompson Canyon region Colorado using monazite dating of foliations preserved<br />

within garnet and staurolite porphyroblastic phases<br />

Ning Qiu<br />

Interpretation of aeromagnetic anomalies of the Sulu ultrahigh-pressure (UHP)<br />

metamorphic belt, eastern China<br />

Svetlana Kokh Combustion metamorphic rocks as a sign of ancient mud volcanoes<br />

Yongmei Zhang<br />

The genetic of the Damiao granodiorite in Siziwangqi and its constraint on the crust<br />

evolution of Inner Mongolia<br />

09:45-10:00 Maria D'Amico<br />

Source parameters evaluation of the 28th December 1908 and 16th January 1975<br />

earthquakes in the Messina Straits (Southern Italy)<br />

10:00-10:15 休 息<br />

10:15-10:30 Fatima El Atrassi*<br />

Pressure and Temperature Conditions recorded by the Beni-Bousera ultramafic body<br />

and the overlying lower-crustal rocks (Rif, Morocco)<br />

10:30-10:45 Meagan Webster<br />

Gondwana terrane assembly in northern Mozambique: A snapshot of crustal processes<br />

in the Monapo Klippe<br />

10:45-11:00<br />

Ndivhuwo Cecilia<br />

Mukosi<br />

Petrogenesis of the Ambohiby Complex Madagascar and the role of the Marion Hot<br />

Spot<br />

11:00-11:15 Vishnevskaya Irina Sr-isotopic characteristic of the typical carbonate Neoproterozoic Siberia sections<br />

11:15-11:30 Tumashov Igor<br />

Lithologic and petrographic characteristic of vend-Palaeozoic sediments of the<br />

11:30-11:45<br />

Qiong Liu<br />

southeast of west Siberia<br />

Elasticity change in Fe2SiO4 spinel and across the olivine-spinel transition in Fe2SiO4<br />

at high P and T by synchrotron X-radiation and ultrasonic interferometry using<br />

multi-anvil apparatus<br />

21

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