机译:波希米亚地块浅层克尔科诺斯-伊泽拉古生物复合体中的多阶段岩浆侵位和渐进应变累积
Institute of Geology and Paleontology, Faculty of Science, Charles University, Albertov 6, Prague 12843, Czech Republic;
Czech Geological Survey, Prague, Czech Republic,institute of Petrology and Structural Geology, Faculty of Science, Charles University, Prague, Czech Republic;
Centre for Geobiology and Department of Earth Science, University of Bergen, Bergen, Norway,Institute of Geology, Academy of Sciences of the Czech Republic, v.v.i., Prague, Czech Republic;
Institute of Geology and Paleontology, Faculty of Science, Charles University, Prague, Czech Republic;
Bohacova 866, Prague, Czech Republic;
机译:波西米亚地块的Krkonose-Jizera Plutonic复杂岩浆结构:花岗岩岩浆室内局部多相流和小规模热力学不稳定性的证据
机译:岩浆停止是瓦里斯卡纳云母的重要进位机制:中波西米亚云母岩体(波西米亚地块)屋顶垂饰的证据
机译:底板沉降使岩浆室内的岩浆流动路径和应变模式:基于磁性织物的西喀尔巴阡?tiavnica火山-岩溶复合体中浅层岩体的模型研究
机译:德卢斯情结中薄层岩浆侵位的多次发作:来自岩浆-流体相互作用的证据吗?
机译:东部蓝岭岩体复合体和相关岩性的结构成因和地层环境,阿拉巴马州的阿巴拉契亚山脉
机译:Synechococcus sp。的表征。菌株PCC 7002自发突变菌株在光系统II核心叶绿素-蛋白质复合物的积累中有缺陷。
机译:浅层带状花岗岩岩体(摩洛哥塔尔科特岩体)的分化和侵位过程中的岩浆-宿主相互作用:对岩浆侵位的影响
机译:复杂多轴加载下的循环应变积累,