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您的检索式：作者名="LIUXiaohan"
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| 1 | Grove Mountains(GRV)99027:A new Martian meteorite显示文摘We report the petrography, mineral chemistry and oxygen isotopic composition of GRV 99027, a new Mar-tian meteorite recently collected during the 16th Chinese Antarctic Research Expedition. This meteorite consists of two textural regions. The interstitial region is characterized by the presence of plagioclase and phosphate, and higher FeO contents of olivine and orthopyroxene, in comparison with the poikilitic region. All of the observations are similar to the three known Martian lherzolites. We classify GRV 99027 as the fourth sample of Martian lherzolite. | LINYangting WANGDaode MIAOBingkui OUYANGZiyuan LIUXiaohan JUYitai | 2003 | Chinese Science Bulletin2003，48，16： | 11 |
| 2 | Sedimentary environments of the Cenozoic sedimentary debris found in the moraines of the Grove Mountains, east Antarctica and its climatic implications显示文摘During the field work of the 1998~1999’s and 1999~2000’s Chinese National Antarctic Research Expedition (CHNARE) in the Grove Mountains, east Antarctica, some Cenozoic sedimentary debris are found in two terminal moraine banks over the blue ice near Harding Mount in the center of this region. All the debris are of characteristics of glaciogenic diamicton and belong to the products of the glacial movements of the East Antarctic Ice Sheet. In this paper, the authors make a detailed study on the sedimentary environments of the sedimentary debris through petrologic, sedimentological, mineralogical, and geo chemical methods. Characteristics of their sedimentary textures and structures, grain size distributions, quartz grains’ surface textures and features, together with their geo chemical compositions all show that these sedimentary rocks are a kind of subglacial lodgement tills which are deposited in the ice sheet frontal area by reactions of glacial movements and glaciogenic melt water. Their palaeoenvironmental implications in revealing the retreat history of East Antarctic Ice Sheet are discussed. The authors draw the conclusion from current study that the glacial frontal of the East Antarctica Ice Sheet might have been retreated to this area during the Pliocene Epoch, which represents a warm climate event accompanied by a large scale ice sheet retreat in Antarctica at that time. | FANGAimin LIUXiaohan LEEJongIk LIXiaoli HUANGFEIXIN | 2004 | Progress in Natural Science:Materials International2004，14，3： | 6 |
| 3 | Compositional Distribution and Growth Mode of Garnet Porphyroblasts during Deformation and Metamorphism显示文摘Although porphyroblast microstmctures play an important role in structural and metamorphic studies, there are still controversies in the interpretation. The focus is how porphyroblasts grow during deformation and metamorphism.In this paper, we introduce a new approach, the Synchrotron Radiation X-Ray Fluorescence, to a hemi-quantitative interpretation of the growth mode of porphyroblasts. The analysis was done at the Beijing Synchrotron Radiation Facility.The specimens were sampled from metapelite of the Baoyintu Group, northern Urad Middle Banner, Inner Mongolia. The new method is successful for determining the microscopic distribution of trace elements in porphybroblasts. The results support the theory of deformation partition, which has been brought forth by Bell and his colleagues, and demonstrate the existence of porphyroblast growth phases and the growth mode of porphyroblasts by hemi-quantitative mineral chemical analysis. The porphyroblast grows stage by stage in the manner of the distribution of a roseleaf and is controlled by deformation. We call the growth stage of porphyroblast a growth phase. | ZHAOGuiping LIUShuwen LIUXiaohan | 2004 | Acta Geologica Sinica(English Edition)2004，78，1： | 1 |
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