...
机译:上部地壳分化过程及其在San Pedro-Linzor火山链(Central Andes)的238U-230款不平衡的作用
Univ Chile Fac Ciencias Fis & Matemat Ctr Excelencia Geotermia Andes CEGA Plaza Ercilla 803 Santiago Chile|Univ Chile Fac Ciencias Fis & Matemat Dept Geol Plaza Ercilla 803 Santiago Chile;
Macquarie Univ Dept Earth & Planetary Sci Sydney NSW 2109 Australia|Univ Adelaide Dept Earth Sci Adelaide SA 5005 Australia;
Univ Catolica Norte Dept Ciencias Geol Avda Angamos 0610 Antofagasta Chile|Univ Cape Town Dept Geol Sci ZA-7700 Rondebosch South Africa;
Univ Catolica Temuco Fac Ingn Dept Obras Civiles & Geol Rudecindo Ortega 02950 Chile;
Univ Cape Town Dept Geol Sci ZA-7700 Rondebosch South Africa;
Univ Chile Fac Ciencias Fis & Matemat Ctr Excelencia Geotermia Andes CEGA Plaza Ercilla 803 Santiago Chile|Univ Chile Fac Ciencias Fis & Matemat Dept Geol Plaza Ercilla 803 Santiago Chile;
Bruker Nano GmbH Studio 2D D-12489 Berlin Germany;
U-series disequilibria; San Pedro - Linzor volcanic chain; U-238 excess; Subduction zone magmatism; Amphibole fractionation;
机译:地壳增厚过程中弧状岩浆的低压演化:智利北部安第斯山脉中部的圣佩德罗-林佐火山链
机译:来自中南部的小火山中心的颅内肌腱U系列不平衡
机译:在San Pedro-Linzor火山链下,北智利下面的电导率分布,采用3-D Magnetelluric建模
机译:中南部安第斯山脉普纳高原内陆地壳形变力学的InSAR观测
机译:新斯科舍省中部边缘的地壳结构以及加拿大东部从火山向非火山的裂谷过渡。
机译:科伦坡海底火山圣托里尼火山场爱琴海弧的独特来源和分化史
机译:安第斯山脉中部(阿根廷门多萨)佩恩火山复合体中的裂隙火山作用,多系火山场和地壳厚度