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431.
W. Kalkreuth N. Sherwood G. Cioccari Z. Corrêa da Silva M. Silva N. Zhong L. Zufa 《International Journal of Coal Geology》2004,57(3-4):167-185
Combining vitrinite reflectance (VR) and fluorescence alteration of multiple macerals (FAMM) analyses provide insights into the chemical nature of vitrinites (i.e., perhydrous vs. orthohydrous vs. subhydrous compositions) in Permian Gondwana coals of the Paraná Basin, Brazil. The FAMM-derived equivalent VR (EqVR) values and relationships with VR can be determined according to calibration curves based largely on Permian Gondwana coals of eastern Australia.The analytical results indicate that vitrinites in the Paraná Basin coals studied generally range from orthohydrous to perhydrous, with interpreted VR suppression ranging up to 0.2% absolute for the most perhydrous case. The EqVR values of the Santa Catarina coals, which range from about 0.85% to 0.95% differ from VR values by about 0.10–0.15% absolute, potentially having significant implications on coal utilization.The causes of vitrinite reflectance suppression in the Paraná Basin coals are as yet poorly understood, but are likely to be related to a combination of factors. 相似文献
432.
ZHAO Guiping LIU Shuwen LIU Xiaohan Computational Geodynamics Laboratory Graduate School of Chinese Academyof Sciences Beijing School of Earth Space Sciences Peking University Beijing Institute of Geology Geophysics Chinese Academy of Sciences Beijing 《《地质学报》英文版》2004,78(1):186-190
Although porphyroblast microstructures 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 相似文献
433.
近年来,中国的各种传媒上不断出现有关夜明珠的报道。引起了广泛的注意,当前市场上出现的夜明珠主要是荧石夜明珠,笔者对荧石夜明珠作了一些初步研究和探讨。发光的原因主要是含稀土元素(rare earth elements)所致,含量可以低至万分数。本文的资料希望能促进对夜明珠问题的深入认识。 相似文献
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荒漠植物花棒耐盐性的傅立叶红外光谱法研究 总被引:6,自引:5,他引:1
试验以荒漠植物花棒幼苗为材料,应用傅立叶红外光谱(FTIR)法研究了NaCl胁迫下花棒叶片主要有机化合物含量和蛋白质结构的变化以及叶片K+和Na+含量。结果表明,叶片Na+、K+含量随着0~255 mM NaCl盐胁迫逐渐增强而变化,导致Na+/K+比值逐渐降低,显示出盐胁迫下花棒幼苗具有”吸钾排纳”特性。花棒幼苗再170 mM NaCl的高浓度胁迫下24 h,叶片中蛋白质、酯类和碳水化合物含量大幅度增加。花棒的蛋白质二级结构中1 665/1 638 cm-1比值的逐渐降低。揭示出花棒植株通过增强蛋白质、酯类和碳水化合物合成代谢调控能力抵御盐胁迫的损伤,而且花棒蛋白质二级结构更趋稳定,与叶片中Na+/K+比值的变化趋势显著相关。因此花棒为了适应高浓度盐胁迫,具有叶片蛋白质、酯类快速合成以及蛋白质构象更趋于稳定的积极响应。 相似文献
438.
地质样品中高精度铬同位素分析纯化技术研究进展 总被引:1,自引:1,他引:0
随着多接收器热电离质谱仪(MC-TIMS)和多接收器电感耦合等离子体质谱仪(MC-ICP-MS)的发展,高精度铬(Cr)同位素测试已成为可能。铬同位素在地球、环境、农业生态和宇宙化学等科学领域中已显示出良好的应用潜力。然而,样品的纯化分离、干扰和仪器质量分馏的校正,依然是制约铬同位素高精度测试的重要因素。本文在近年来铬同位素分析技术最新进展的基础上,结合本课题组已有的研究,对陨石、地质和环境等各类样品中铬同位素的分离纯化方法、MC-ICP-MS测试中干扰与质量歧视校正等进行了详细综述。本文认为,阴阳离子树脂交换联用与过硫酸钾等强氧化剂的结合,可以进行低铬高基质样品的有效纯化,是一种较为普适性的纯化方法。使用铬同位素双稀释剂校正质量歧视效应,在MC-ICP-MS的中高分辨与静态测量模式下,不仅可以有效分开多原子离子的干扰,而且也可以进行高精度铬同位素分析,其δ~(53/52)Cr的分析精度与TIMS相当,可以达到0.04‰(2SD),且最低测试浓度可低至10ng,能够实现超微量铬的同位素分析。 相似文献
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The deeply buried reservoirs (DBRs) from the Lijin, Shengtuo and Minfeng areas in the northern Dongying Depression of the Bohai Bay Basin, China exhibit various petroleum types (black oil-gas condensates) and pressure systems (normal pressure-overpressure) with high reservoir temperatures (154–185 °C). The pressure-volume-temperature-composition (PVTX) evolution of petroleum and the processes of petroleum accumulation were reconstructed using integrated data from fluid inclusions, stable carbon isotope data of natural gas and one-dimensional basin modeling to trace the petroleum accumulation histories.The results suggest that (1) the gas condensates in the Lijin area originated from the thermal cracking of highly mature kerogen in deeper formations. Two episodes of gas condensate charging, which were evidenced by the trapping of non-fluorescent gas condensate inclusions, occurred between 29-25.5 Ma and 8.6–5.0 Ma with strong overpressure (pressure coefficient, Pc = 1.68–1.70), resulting in the greatest contribution to the present-day gas condensate accumulation; (2) the early yellow fluorescent oil charge was responsible for the present-day black oil accumulation in well T764, while the late blue-white oil charge together with the latest kerogen cracked gas injection resulted in the present-day volatile oil accumulation in well T765; and (3) the various fluorescent colors (yellow, blue-white and blue) and the degree of bubble filling (Fv) (2.3–72.5%) of the oil inclusions in the Minfeng area show a wide range of thermal maturity (API gravity ranges from 30 to 50°), representing the charging of black oil to gas condensates. The presence of abundant blue-white fluorescent oil inclusions with high Grain-obtaining Oil Inclusion (GOI) values (35.8%, usually >5% in oil reservoirs) indicate that a paleo-oil accumulation with an approximate API gravity of 39–40° could have occurred before 25 Ma, and gas from oil cracking in deeper formations was injected into the paleo-oil reservoir from 2.8 Ma to 0 Ma, resulting in the present-day gas condensate oil accumulation. This oil and gas accumulation model results in three oil and gas distribution zones: 1) normal oil reservoirs at relatively shallow depth; 2) gas condensate reservoirs that originated from the mixture of oil cracking gas with a paleo-oil reservoir at intermediate depth; and 3) oil-cracked gas reservoirs at deeper depth.The retardation of organic matter maturation and oil cracking by high overpressure could have played an important role in the distribution of different origins of gas condensate accumulations in the Lijin and Minfeng areas. The application of oil and gas accumulation models in this study is not limited to the Dongying Depression and can be applied to other overpressured rift basins. 相似文献