The Paleoproterozoic was a critical time in whether modern-style plate tectonics had become globally dominant(e.g.,Wan et al.,2020).The Capricorn Orogen witnessed the assembly of the Pilbara and Yilgarn Cratons and an...The Paleoproterozoic was a critical time in whether modern-style plate tectonics had become globally dominant(e.g.,Wan et al.,2020).The Capricorn Orogen witnessed the assembly of the Pilbara and Yilgarn Cratons and an exotic microcontinent,the Glenburgh Terrane,to form the West Australia Craton(WAC)through two collisional orogenic events,the 2215–2145 Ma Ophthalmian and 2005–1950 Ma Glenburgh Orogenies(Johnson et al.,2013;Fig.1).Compared to other Proterozoic orogenic belts in Australia,the Capricorn Orogen preserves‘complete'opposing continental margin successions,together with intervening arc fragments associated with oceanic closure and foreland basins associated with collisional loading(Cawood et al.,2009).展开更多
The continental crustobody of China is composed of three regional crustobodies, i. e., the Cathaysian crustobody, the West China crustobody and the South Tibet crustobody. This paper gives their mass models and elemen...The continental crustobody of China is composed of three regional crustobodies, i. e., the Cathaysian crustobody, the West China crustobody and the South Tibet crustobody. This paper gives their mass models and element abundance values and discusses their regional abundance characteristics from metallogenic elernents, heat source elements and lanthanide elements. The conclusion is that their geochemical backgrounds are quite different from each other.展开更多
文摘The Paleoproterozoic was a critical time in whether modern-style plate tectonics had become globally dominant(e.g.,Wan et al.,2020).The Capricorn Orogen witnessed the assembly of the Pilbara and Yilgarn Cratons and an exotic microcontinent,the Glenburgh Terrane,to form the West Australia Craton(WAC)through two collisional orogenic events,the 2215–2145 Ma Ophthalmian and 2005–1950 Ma Glenburgh Orogenies(Johnson et al.,2013;Fig.1).Compared to other Proterozoic orogenic belts in Australia,the Capricorn Orogen preserves‘complete'opposing continental margin successions,together with intervening arc fragments associated with oceanic closure and foreland basins associated with collisional loading(Cawood et al.,2009).
文摘以“红阳”猕猴桃为试材,通过气相迁移离子色谱(gas chromatography-ion mobility spectrometry,GC-IMS)技术分析比较灭菌后果汁(YL)、发酵对照组(CK)、植物乳杆菌发酵果汁(PL)挥发性风味物质组成,并采用偏最小二乘判别分析(Partial least squares-discrimination analysis,PLS-DA)筛选不同处理样品的差异物质,探讨乳酸菌发酵对“红阳”猕猴桃汁挥发性风味物质组成的影响。结果表明,该研究所选用菌株(Lactobacillus plantanum B-1)应用于猕猴桃果汁发酵在24 h内菌落数由6.21 lg CFU/mL快速上升至8.60 lg CFU/mL,总酸由原来的0.60%增加至1.33%,发酵性能良好。GC-IMS结合PLS-DA分析结果表明,植物乳杆菌发酵可提高(E)-2-己烯醛、己醇、芳樟醇、乙酸乙酯、丁酸乙酯,丙酮、4-庚酮、2-壬酮等含量,增加果汁果香味,减少1,8-桉叶素、(E)-2-己烯醇、己醛等猕猴桃特征风味物质的损失,抑制乙醇、糠醛等对风味产生不良影响的物质生成,从而提升猕猴桃果汁风味品质。该研究为植物乳杆菌在猕猴桃果汁产品中应用提供了理论支撑。
文摘The continental crustobody of China is composed of three regional crustobodies, i. e., the Cathaysian crustobody, the West China crustobody and the South Tibet crustobody. This paper gives their mass models and element abundance values and discusses their regional abundance characteristics from metallogenic elernents, heat source elements and lanthanide elements. The conclusion is that their geochemical backgrounds are quite different from each other.
