国际学生入学条件
Applicants to our graduate program commonly have a Bachelor's degree in Earth Sciences or closely related discipline, but the multidisciplinary nature of our program allows for entry from other backgrounds as well. Students entering the graduate program in Earth and Climate Sciences typically have completed at least one year of chemistry, physics, and calculus, as well as several courses in Earth or environmental sciences beyond the introductory level. Students who have not completed these basic requirements may be admitted, but may be required to complete specific courses to fulfill deficiencies. Deficiencies are determined on an individual basis by the student's chosen advisor, and depend on the research topic and subdiscipline chosen by the student.
Official transcript of all previous college or university work
The School has no formal minimum GRE or GPA requirements.
Before submitting an application, students should contact individual faculty members within the School to determine if:
their interests align with current faculty research programs
if individual faculty are interested in mentoring additional students
what resources are available to pursue research activities
IELTS - 6.5
TOEFL IBT - 80
Duolingo English Test - 105
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IDP—雅思考试联合主办方
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雅思考试总分
6.5
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雅思考试指南
- 雅思总分:6.5
- 托福网考总分:80
- 托福笔试总分:550
- 其他语言考试:Pearson Test of English Academic - 60
CRICOS代码:
申请截止日期: 请与IDP顾问联系以获取详细信息。
课程简介
Rocks and landforms at Earth's surface, potentially hazardous volcanic and seismic activity, the response of Earth's surface to icecaps that come and go with changing climate, and the slow but inexorable movement of continents all result from the interaction of physical and chemical processes taking place throughout Earth's crust and mantle. With international interest and funding directed towards addressing both basic research questions and applied problems, the broad fields of geodynamics, structural geology, mineralogy and petrology are mainstays of geoscience research.<br><br>Our ongoing and new capacity for microanalysis, including optical microscopy, energy- and wavelength-dispersive spectrometry, cathodoluminescence, and electron backscatter diffraction, along with grain- through orogen-scale numerical modeling and supercomputer applications, allow us to develop groundbreaking ideas related to coupled physical and chemical processes that shape Earth's surface and drive evolution of its lithosphere.<br><br>Our research program spans spatial scales from micrometers in individual mineral grains (deformation mechanisms, mineral chemistry, microstructures) to hundreds of kilometers in mountain belts (tectonic history, magmatism, structural development, and coupling of surface and deep processes). We study events that occurred from 4 billion years ago at the dawn of Earth's history to those active today. We make observations of the natural world, using field, analytical, geochemical and geophysical datasets, and explain these observations using basic physical and chemical principles.<br><br>We employ numerical and analogue modeling to test our explanations and conceptual predictions. Our most active research threads center on relating strain to surface evolution, mountain-scale dynamics, mid- to lower-crustal rheology, elastic anisotropy, earthquake geology, microstructural evolution, magma dynamics, pressure-temperature and chemical evolution of metamorphic rocks, stable isotope fractionation and mineral paragenesis
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