机译:在裂缝结晶岩石中微生物硫酸盐减少后形成的前所未有的3434份富集硫酸盐
Department of Biology and Environmental ScienceLinn?us UniversityKalmar Sweden;
Department of GeosciencesSwedish Museum of Natural HistoryStockholm Sweden;
Department of GeobiologyGeoscience Centre G?ttingen of the Georg‐August UniversityG?ttingen Germany;
Department of GeosciencesUniversity of ArizonaTucson Arizona;
Department of Biology and Environmental ScienceLinn?us UniversityKalmar Sweden;
Department of Earth SciencesUniversity of GothenburgGothenburg Sweden;
Department of Biology and Environmental ScienceLinn?us UniversityKalmar Sweden;
Department of Geological SciencesStockholm UniversityStockholm Sweden;
Department of Biology and Environmental ScienceLinn?us UniversityKalmar Sweden;
continental crust; deep biosphere; microbial sulfate reduction; pyrite; sulfur isotopes;
机译:在裂缝结晶岩石中微生物硫酸盐减少后形成的前所未有的3434份富集硫酸盐
机译:裂缝结晶基岩中低温硫铁矿的微观同位素可变性 - Fe(II)(AQ)/硫铁矿之间的大型Fe同位素分馏和Fe-S同位素的缺失
机译:晶体基底中断裂方解石和黄铁矿的微生物活动指示对低温微量元素迁移率的影响
机译:研究非饱和堆模拟柱系统中富含黄铁矿的Waste石矿物表面上的微生物代谢活性
机译:低孔隙度结晶岩中的破裂萌生和扩展:对开挖损伤区(EDZ)力学的影响
机译:Fe(III)-RICH岩石流动条件下Fe(III)(氢)氧化物的水文改变及增强微生物还原溶解:对洞穴形成过程的贡献
机译:硫铁矿和溶解硫酸盐中δ34S的变化揭示了深基岩骨折中的减硫细菌活性