The Okavango Delta is a large low gradient alluvial fan or"Inland Delta"located in north western Botswana.Tlie area includes per manent swamps which cover approximately 600.000 hectare along with up to 1.2 m...The Okavango Delta is a large low gradient alluvial fan or"Inland Delta"located in north western Botswana.Tlie area includes per manent swamps which cover approximately 600.000 hectare along with up to 1.2 mil lion hectare of seasonally flooded grass land The inscribed World Heritage property encompasses an ai ea of 2.023,590 hectaie with a iDiiffer zone of 2,286,630 hectare.展开更多
Ti-rich garnet is found within calcitic ijolite from the Oka carbonatite complex in Canada, which is characterized by 58%-73% andradite component（2.12 wt.%-4.18 wt.% TiO_2） and classified as melanite. The garnet dis...Ti-rich garnet is found within calcitic ijolite from the Oka carbonatite complex in Canada, which is characterized by 58%-73% andradite component（2.12 wt.%-4.18 wt.% TiO_2） and classified as melanite. The garnet displays complex zoning and contains abundant high field strength elements（HFSEs） and rare earth elements（REEs）. Three groups（Ⅰ, Ⅱ, Ⅲ） have been identified based on their petrographic nature. Compared to groups Ⅱ and Ⅲ, Group Ⅰ garnet cores contain higher TiO_2, Mg O, HFSE, and REE and lower SiO_2 abundances. The distinct chemical and petrographic signatures of the investigated garnets cannot be attributed to simple closed system crystallization, but they are consistent with the multi-pulse magma mixing. Combined with previously reported U-Pb ages for apatite from the calcitic ijolite, at least three stages of magma evolution and subsequent mixing have been involved in the generation of calcitic ijolite at Oka. The early-formed melt that generated Group I garnet core was later mixed with at least two small-volume, more evolved melts. The intermediate stage melt formed the remaining garnet along with some pyroxene, calcite, nepheline, and apatite at 127±3.6 Ma. The youngest, most evolved melt generated the majority of pyroxene, calcite, nepheline, and apatite within the calcitic ijolite at 115±3.1 Ma.展开更多
文摘采用二代测序(next-generation sequencing,NGS)技术,对上海生物制品研究所有限责任公司(简称SIBP)2015—2017这3个年度生产的Oka株水痘疫苗进行深度测序,从分子水平分析疫苗质量的一致性,并与不同厂家疫苗/毒种进行比较,分析它们之间的遗传特征相关性。结果显示,3个年度生产的水痘疫苗中平均有77个位点的疫苗型位点检出频率(proportion of vaccine-type allele,Pv)≥10%,至少在两批疫苗中出现Pv≥10%的位点数共76个,两两之间Pv最大差值<10%,与平均值的最大差值为<5%。共有40个位点的Pv均值≥30%,其中19个位点导致氨基酸残基变异;15个位于ORF62区域。筛选出35个位点,比较5个公司水痘疫苗/毒种的Oka株病毒基因序列,结果显示它们之间存在相关性,同时存在一定的差异。研究表明,SIBP不同年度生产的水痘疫苗Oka株病毒具有良好的分子水平上的一致性,为疫苗质量管理与市场监督提供了方法和基础数据。
文摘The Okavango Delta is a large low gradient alluvial fan or"Inland Delta"located in north western Botswana.Tlie area includes per manent swamps which cover approximately 600.000 hectare along with up to 1.2 mil lion hectare of seasonally flooded grass land The inscribed World Heritage property encompasses an ai ea of 2.023,590 hectaie with a iDiiffer zone of 2,286,630 hectare.
基金supported by the National Natural Science Foundation of China (No. 41402046)the Fundamental Research Funds for the Central Universities (No. 2015219102)+1 种基金the special fund from the State Key Laboratory of Geological Processes and Mineral Resourcesfinancial support during her doctoral dissertation from the University of Notre Dame
文摘Ti-rich garnet is found within calcitic ijolite from the Oka carbonatite complex in Canada, which is characterized by 58%-73% andradite component（2.12 wt.%-4.18 wt.% TiO_2） and classified as melanite. The garnet displays complex zoning and contains abundant high field strength elements（HFSEs） and rare earth elements（REEs）. Three groups（Ⅰ, Ⅱ, Ⅲ） have been identified based on their petrographic nature. Compared to groups Ⅱ and Ⅲ, Group Ⅰ garnet cores contain higher TiO_2, Mg O, HFSE, and REE and lower SiO_2 abundances. The distinct chemical and petrographic signatures of the investigated garnets cannot be attributed to simple closed system crystallization, but they are consistent with the multi-pulse magma mixing. Combined with previously reported U-Pb ages for apatite from the calcitic ijolite, at least three stages of magma evolution and subsequent mixing have been involved in the generation of calcitic ijolite at Oka. The early-formed melt that generated Group I garnet core was later mixed with at least two small-volume, more evolved melts. The intermediate stage melt formed the remaining garnet along with some pyroxene, calcite, nepheline, and apatite at 127±3.6 Ma. The youngest, most evolved melt generated the majority of pyroxene, calcite, nepheline, and apatite within the calcitic ijolite at 115±3.1 Ma.
