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Shouji Kihara Kenichi Hoshino Makoto Watanabe Hirotsugu Nishido Shunso Ishihara 《Resource Geology》2005,55(2):123-129
Abstract. The Umanotani-Shiroyama pegmatite deposits, the largest producer of K-feldspar and quartz in Japan, are of typical granitic pegmatite. Ilmenite-series biotite granite and granite porphyry, hosting the ore deposits, and biotites separated from these rocks yielded K-Ar ages ranging from 89.0 to 81.4 Ma and 95.2 to 93.7 Ma, respectively. Muscovite and K-feldspar separated from the ore zone yielded K-Ar ages with the range of 96.2 to 93.1 Ma and 87.3 to 80.7 Ma, respectively. Muscovites from quartz-muscovite veins in the ore zone and in the granite porphyry yielded K-Ar ages of 90.4 and 76.3 Ma, respectively. K-feldspar is much younger in age than coexisting muscovite. It is noted that the K-Ar ages of biotite separates and the whole-rock ages are identical to those of muscovite and K-feldspar in the ore zone, respectively. These time relations, as well as field occurrence, indicate that the formation of the pegmatite deposits at the Umanotani-Shiroyama mine is closely related in space and time to a series of granitic magmatism of ilmenite-series nature. Using closure temperatures of the K-Ar system for biotite and K-feldspar (microcline), cooling rate of the pegmatite deposits is estimated to be about 82C/m.y. at the beginning, but slowed down to about 15C/m.y. in the later period. 相似文献
2.
中国地质调查局2008年在南祁连盆地木里冻土区采集到了中国陆域第一例天然气水合物实物样品,对于天然气水合物的气体来源存在不同的认识。利用新完钻3口井样品的化验分析结果,分析了中侏罗统和上三叠统烃源岩有机地球化学特征。结果表明,中侏罗统江仓组、木里组煤系地层烃源岩有机质丰度较高,TOC(总有机碳含量)大于1%的样品占78.9%;氯仿沥青"A"含量大于0.1%的占总数的72.2%;有机质类型以Ⅱ_2、Ⅱ_1型为主;镜质体反射率R_o多介于0.7%~1.2%之间;71个样品生烃潜量平均值为8.8mg/g,总体处于生烃高峰期的生油阶段或凝析油阶段,属于好、很好烃源岩,为天然气水合物主力生烃层系。上三叠统尕勒得寺组亦为煤系地层烃源岩,TOC含量大于1%的样品占76.9%;氯仿沥青"A"含量小于0.05%;有机质类型以Ⅲ、Ⅱ_1型为主;镜质体反射率Ro介于1.1%~1.77%之间;总体处于生湿气或干气阶段,但由于构造抬升影响其生烃潜量,平均值仅为0.35mg/g,当前整体生烃能力较差,为非烃源岩或较差烃源岩,对天然气水合物成藏贡献不大。 相似文献
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发现于德国南部的早侏罗世土亚辛期的海螂蛤页岩相沉积是中生代最早一次,也是唯一保存在大陆地层中的全球性大洋缺氧事件的典型代表。近年中国羌塘盆地已相继发现4处海螂蛤页岩相地层。北羌塘天然气水合物钻探试验井QK-5井钻遇含海螂蛤页岩相特有化石组合的地层,厚度逾150m,是迄今所知羌塘盆地纬度最高的海螂蛤页岩相产地,其他3处分布在羌塘盆地中间隆起带以南的双湖和色哇等地。海螂蛤页岩相的分布纵贯南、北羌塘,意味着羌塘盆地在早侏罗世并没有受到中间隆起带的制约而分成南、北2个独立的沉积凹陷。北羌塘西部白龙冰河、半岛湖一带与东部雀莫措、雁石坪一带的早侏罗世沉积相截然不同,形成早侏罗世西海东陆的沉积格局。海螂蛤页岩相在羌塘盆地的发现,有助于进一步认识中生代羌塘盆地沉积和古海洋演化历史。该区以海螂蛤黑色页岩为代表的富碳沉积无论是分布面积还是沉积厚度都十分可观,对盆地的天然气水合物、页岩气及常规油气勘探具有重要的意义。 相似文献
4.
中国地质调查局油气资源调查中心牵头组织实施的“非常规油气地质调查工程”,开展了黑龙江省鸡西地区煤系气地质调查、松辽盆地及外围油页岩地质调查、松辽盆地西斜坡油砂原位试采工程、陆域天然气水合物地质调查与祁连山木里天然气水合物野外长期观测站建设、陕西关中地区氦气地质调查和非常规油气资源国情调研等工作,获取了大量基础数据,取得了黑鸡地1井、黑鸡地3井、黑鸡地4井等一系列突破性成果和重要进展,初步掌握了我国油页岩、油砂、陆域天然气水合物、氦气以及鸡西盆地煤系气等非常规油气资源潜力。该工程在煤系气、油页岩、氦气等领域产生重要影响,提振了非常规油气勘探开发信心,推动了科技创新与地质调查深度融合,促进了非常规油气学科发展。 相似文献
5.
Kuniaki Kihara 《Physics and Chemistry of Minerals》1995,22(4):223-232
Disorder models of oxygen positions in P63/ mmc, C2221 and P212121 tridymites were given in applying geometrical and lattice dynamical calculations. Sixmembered rings of rigid SiO4 units are all collapsed in these forms; with silicon atoms fixed, SiO4 units can take six different orientations in forming tridymite frameworks in both the P63/mmc and C2221 forms, and three orientations in the P212121 form. Atomic distances and angles obtained from the distance least-squares method are about equal for the three forms: 〈Si-O〉 (mean Si-O) = 1.611 Å, 〈O-O〉 = 2.629 Å, and 〈Si-O-Si〉 = 147°. Domain formation models are given for the three forms. The tridymite framework structures may possibly undergo lattice vibrations with low frequencies in two kinds of pair-wise rotational modes of SiO4 units joined by the apical oxygen atoms, at the Γ-point: one is around 〈100〉 (or 〈210〉 for the hexagonal case), and the other is around 〈010〉. As temperature approaches the hexagonal-orthorhombic transition from below, the rotational mode around 〈100〉 remarkably softens at the Γ-point. The behavior of the atoms at the hexagonal-orthorhombic transition is explained in terms of a coupled softening of the two rotational modes of neighboring local domains in different orientations. 相似文献
7.
多时相耕地覆盖提取和变化分析：一种结合遥感和空间统计的时空上下文方法 总被引：1，自引：0，他引：1
基于多时相影像的耕地提取和变化分析是有效管理和保护耕地资源的重要手段。然而就多时相耕地的分类提取而言,现有方法对于多时相影像中地物的时空特征表达和时空上下文关系建模存在着局限性,导致耕地的提取精度不佳;其次,对于耕地的变化分析,现有方法往往只关注基于行政单元的耕地面积统计变化,而对耕地变化在空间上的相关性分布特点考虑较少。因此,本文首先提出了一种时空上下文分类方法,综合表达和利用多时相影像中地物的光谱、纹理和空间等特征,建模时空维度上地物间在特征和语义上的上下文关系,来提高耕地覆盖分类的精度;其次,基于耕地覆盖的提取结果,在规则格网和行政区划单元上,采用GIS空间统计方法分析耕地变化的空间相关性特点;最后,以北京市顺义区为例,以2015—2019年的多时相Sentinel-2影像为数据源对本文方法进行验证。结果表明,与常见的2种多时相影像分类方法相比,本文方法在多时相耕地分类上精度最高,平均用户精度和制图精度分别达到91.21%和90.53%,所有类别的总体精度为90.79%。这表明本文方法能精确提取多时相耕地覆盖信息。通过对耕地变化的空间分布特点进行分析,发现2015—2019年顺义区耕地变化存在区域聚集现象,主要呈现为集中减少特点,其中赵全营镇、高丽营镇、木林镇和杨镇地区耕地的聚集性减少较为明显,说明这些地区的耕地侵占和减少问题比较严重。 相似文献
8.
针对QK-3井取得的曲色组泥页岩、油页岩以及液态油苗进行了有机地球化学特征分析,探讨曲色组烃源岩与液态油苗的亲缘性。研究表明：QK-3井曲色组泥岩及油页岩达一般—好烃源岩标准,有机质类型多为Ⅰ及Ⅱ1型,处于成熟阶段;油页岩、油苗样品生物标志物对比表明,二者形成环境及成熟度特征较为接近,具有很好的可比性,在曲色组中发现的油苗与该组烃源岩有着较好的亲缘关系,油苗源于曲色组油页岩等烃源岩。综合烃源岩有机地球化学特征及曲色组分布范围与沉积厚度认为,下侏罗统曲色组泥质烃源岩的生烃能力属于较好级别,是研究区内最主要的烃源岩,具有较好的勘探潜力。 相似文献
9.
XIAO Rui ZHU youhai LU Zhenquan LIU Hui PANG Shouji ZHANG Shuai FAN Dongwen WANG Weichao 《中国地质调查》2014,7(4):20-27
Harlahu Depression is basically a geological blank area now. Few studies on the formation and distribution of natural gas hydrate have been published, especially the research and understanding of natural gas hydrate reservoir in this area. The borehole QH-2 is located in the western part of Harlahu Depression of South Qilian Basin, and it was the first deep drilling hole for natural gas hydrate investigation in this area, in which Quaternary,Neogene—Paleogene and Triassic strata were drilled. The authors took the core of Triassic reservoir in well QH-2 as the research object to study the reservoir characteristics of Harlahu Depression, through the thin section observation of rock, porosity, permeability, rock density, casting thin section and other physical property tests, as well as the logging data. The research shows that Triassic reservoir of well QH-2 is widely distributed with great thickness. However, the physical property of the reservoir is poor, and most parts of the reservoir were unconventional reservoirs. The fractures are not developed, so it is difficult to form fracture type hydrate and pore type hydrate in the consolidated rock stratum similar to Muli area. While, the thick Quaternary loose sediments and Tertiary strata with relatively developed fissures were developed under the permafrost regions in this area, which may provide a better reservoir space for the formation of natural gas hydrate. 相似文献
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