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61.
正1研究目的(Objective)湖北宜昌王家湾是全球上奥陶统赫南特阶底界全球界线层型剖面所在地,也是世界上开展奥陶系和志留系界线对比研究的典型地区,具有很高的地层学研究水平。该地奥陶系五峰组—志留系龙马溪组下部以碳硅泥质页岩发育为特点,沉积连续,化石丰富,具有与中国已经建成的重庆涪陵焦石坝和长宁威远国家级页岩气勘探示范区页岩气勘探主力层系相似的地层和古生物发育特点。区域构造稳定,地层产状平缓,页岩气富集地质条件优越,但志留系页岩气的  相似文献   
62.
ABSTRACT

The Guichi ore-cluster district in the Lower Yangtze River Metallogenic Belt hosts extensive Cu–Au–Mo polymetallic deposits including the Tongshan Cu–Mo, Paodaoling Au, Matou Cu–Mo, Anzishan Cu–Mo, Guilinzheng Mo and Zhaceqiao Au deposits, mostly associated with the late Mesozoic magmatic rocks, which has been drawn to attention of study and exploration. However, the metallogenic relationship between magmatic rocks and the Cu–Au-polymetallic deposits is not well constrained. In this study, we report new zircon U–Pb ages, Hf isotopic, and geochemical data for the ore-bearing intrusions of Guichi region. LA-ICP-MS U–Pb ages for the Anzishan quartz diorite porphyrite is 143.9 ± 1.0 Ma. Integrated with previous geochronological data, these late Mesozoic magmatic rocks can be subdivided into two stages of magmatic activities. The first stage (150–132 Ma) is characterized by high-K calc-alkaline intrusions closely associated with Cu–Au polymetallic ore deposits. Whereas, the second stage (130–125 Ma) produced granites and syenites and is mainly characterized by shoshonite series that are related to Mo–Cu mineralization. The first stage of magmatic rocks is considered to be formed by partial melting of subducted Palaeo-Pacific Plate, assimilated with Yangtze lower crust and remelting Meso-Neoproterozoic crust/sediments. The second stage of magmatism is originated from partial melting of Mesoproterozoic-Neoproterozoic crust, mixed with juvenile crustal materials. The depression cross to the uplift zone of the Jiangnan Ancient Continent forms a gradual transition relation, and the hydrothermal mineralization composite with two stages have certain characteristics along the regional fault (Gaotan Fault). Guichi region results from two episodes of magmatism probably related to tectonic transition from subduction of Palaeo-Pacific Plate to back-arc extensional setting between 150 and 125 Ma, which lead to the Mesozoic large-scale polymetallic mineralization events in southeast China.  相似文献   
63.
川北地区寒武系筇竹寺组钙质结核泥页岩中早成岩期钙质结核较发育,结核裂缝中见多期次矿物充填。为揭示钙质结核裂缝形成机理,本次结合岩石学特征及地球化学特征等开展系统研究。川北筇竹寺组钙质结核裂缝中见三~四期矿物充填。第一期微晶方解石表面较脏,阴极发光暗淡,δ13C_(PDB)、δ18O_(PDB)平均值分别为-4.26‰及-7.69‰;第二期为细—中晶粒状方解石充填,阴极发光为橘黄色,流体包裹体均一温度为平均值为86.4℃,δ13C_(PDB)、δ18O_(PDB)平均值分别为-3.15‰及-7.41‰;第三期为粗晶方解石充填阴极发光暗淡,流体包裹体均一温度平均值为96.6℃,δ~(13)C_(_(PDB))、δ~(18)O_(_(PDB))平均值分别为-1.73‰及-10.28‰;第四期为重晶石充填。结合区域构造史—热演化史分析表明,钙质结核裂缝中四期充填物分别指示早期脱水、烃源岩早成熟期生烃、加里东构造运动抬升释压及深埋藏期硫酸盐热还原作用事件。  相似文献   
64.
Some Au deposits in southern Anhui Province have recently been found to be closely associated with Late Mesozoic intrusions. Typical examples include the Huashan Au (Sb) deposit and Au deposits at Zhaojialing, Wuxi, and Liaojia. In order to understand the mechanisms that led the formation of these Au deposits, we make detailed reviews on the geological characteristics of these Au deposits. Specifically, we present new LA-ICP-MS zircon U–Pb dating, along with elemental and Hf isotopic data from the Huashan Au (Sb) deposit. Our data suggests that the Huashan ore-related intrusions were emplaced during the Late Jurassic and Early Cretaceous periods (144–148 Ma). They are characterized by arc-magma features and high oxygen fugacity and are rich in inherited zircons. Zircon U–Pb ages and Lu–Hf isotopes from intrusions suggest that Proterozoic juvenile lithosphere is the main source of these intrusions. The regional geological history implies that lithosphere beneath southern Anhui was produced during a Proterozoic subduction and was fertilized with Au (Cu) in the process. Integrated with the results of previous studies, we inferred that Late Mesozoic intrusions formed by the remelting of the lithosphere could provide the metal endowment for the Au-rich deposits in southern Anhui.  相似文献   
65.
All BeiDou navigation satellite system (BDS) satellites are transmitting signals on three frequencies, which brings new opportunity and challenges for high-accuracy precise point positioning (PPP) with ambiguity resolution (AR). This paper proposes an effective uncalibrated phase delay (UPD) estimation and AR strategy which is based on a raw PPP model. First, triple-frequency raw PPP models are developed. The observation model and stochastic model are designed and extended to accommodate the third frequency. Then, the UPD is parameterized in raw frequency form while estimating with the high-precision and low-noise integer linear combination of float ambiguity which are derived by ambiguity decorrelation. Third, with UPD corrected, the LAMBDA method is used for resolving full or partial ambiguities which can be fixed. This method can be easily and flexibly extended for dual-, triple- or even more frequency. To verify the effectiveness and performance of triple-frequency PPP AR, tests with real BDS data from 90 stations lasting for 21 days were performed in static mode. Data were processed with three strategies: BDS triple-frequency ambiguity-float PPP, BDS triple-frequency PPP with dual-frequency (B1/B2) and three-frequency AR, respectively. Numerous experiment results showed that compared with the ambiguity-float solution, the performance in terms of convergence time and positioning biases can be significantly improved by AR. Among three groups of solutions, the triple-frequency PPP AR achieved the best performance. Compared with dual-frequency AR, additional the third frequency could apparently improve the position estimations during the initialization phase and under constraint environments when the dual-frequency PPP AR is limited by few satellite numbers.  相似文献   
66.
Zhang  Xiaohong  Tao  Xianlu  Zhu  Feng  Shi  Xiang  Wang  Fuhong 《GPS Solutions》2018,22(3):1-11
GPS Solutions - Tropical cyclones are a serious natural disaster concern in Australia due to El Niño and La Niña phenomena. However, little attention has been paid to the ionospheric...  相似文献   
67.
The objective of this study was to analyze the response of runoff in the area of runoff yield of the upstream Shiyang River basin to climate change and to promote sustainable development of regional water resources and ecological environment. As the biggest tributary of the Shiyang River, Xiying River is the only hydrological station (Jiutiaoling) that has provincial natural river and can achieve long time series monitoring data in the basin. The data obtained from this station is representative of natural conditions because it has little human activites. This study built a regression model through identifying the characteristics of runoff and climate change by using Mann-Kendall nonparametric statistical test, cumulative anomaly, and correlation analysis. The results show that the average annual runoff is 320.6 million m3/a with the coefficient of variation of 0.18 and shows slightly decrease during 1956–2020. It has a significant positive correlation the average annual precipitation (P<0.01). Runoff is sensitive to climate change, and the climate has becoming warm and wet and annual runoff has entering wet period from 2003. Compared to the earlier period (1955–2000), the increases of average annual temperature, precipitation and runoff in recent two decades were 15%, 9.3%, and 7.8%, respectively. Runoff in the Shiyang River is affected by temperature and precipitation among climate factors, and the simulation results of the runoff-climate response model (R = 0.0052P ? 0.1589T + 2.373) indicate that higher temperature leads to a weakening of the ecological regulation of surface runoff in the flow-producing area.  相似文献   
68.
Nie  Yufeng  Shen  Yunzhong  Pail  Roland  Chen  Qiujie  Xiao  Yun 《Surveys in Geophysics》2022,43(4):1169-1199
Surveys in Geophysics - The gravity field recovery from GRACE (Gravity Recovery and Climate Experiment) mission data is contaminated by both observation noise and dynamic force errors, especially...  相似文献   
69.
地震是造成人员死亡最严重的自然灾害之一,震后对人员死亡等灾情的快速评估是地震应急响应和救援的关键。总结经验发现,在地震前进行预评估工作是提高震后灾情快速评估精度和时效性的有效手段。通过对62次发生在我国西南地区的历史震例分析后发现,当地震震级小于4.5级时,基本不会造成人员死亡情况。本研究利用我国云南和四川部分区县的实地调研数据,发现地震人员死亡数与震级存在指数函数关系,由此构建了针对各个区县的地震人员死亡人数指数函数估算模型,并计算了回归系数。基于该模型,获得了5.0~8.0级地震人员死亡数查找表(以0.5级为间隔),用于辅助震后快速评估工作。  相似文献   
70.
研究目的】不同页岩岩相的矿物组分、含气性和可压性等的差异,决定不同岩相的开发潜力不同,页岩岩相的划分及评价对找寻页岩气勘探开发甜点具有重要指导意义。【研究方法】基于钻井、岩心和分析测试资料,综合利用地质理论结合硅质矿物-黏土矿物-碳酸盐矿物含量三端元图解,对鄂西宜昌斜坡带上奥陶统五峰组—下志留统龙马溪组下段含气页岩岩相进行划分,结合有机碳含量、含气量、岩心镜下特征等划分优势岩相。优选有机质丰度、硅质矿物含量、黏土矿物含量3项指标与页岩含气量进行相关性分析,建立了五峰组—龙马溪组含气页岩优势岩相的分级标准。【研究结果】研究区优势岩相均为II类优势岩相,II1类(最优)优势岩相为S-2混合硅质页岩相和S-3含黏土硅质页岩相,位于龙马溪组一亚段和五峰组上段,厚6 m;II2类(次优)优势岩相为S硅质页岩相,位于五峰组下段,厚4 m。【结论】宜昌斜坡带和涪陵地区具有相似的岩相垂向演化序列,优势岩相均位于五峰组—龙马溪组一亚段,但同一岩相组合的页岩厚度和品质差异较大,发生在鲁丹阶早期的湘鄂西水下隆起和鲁丹阶晚期的水下隆起是造成宜昌地区优势岩相的厚度和品质均要差于涪陵地区的主要原因。创新点:建立五峰组—龙马溪组含气页岩优势岩相的分级标准,提出龙马溪组一亚段和五峰组是优势岩相发育层位。  相似文献   
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