Large-scale stratigraphic architecture and sequence analysis of an early Pleistocene submarine canyon fill,Monte Ascensione succession (Peri-Adriatic basin,eastern central Italy)     

Claudio Di Celma  Riccardo Teloni  Andrea Rustichelli 《International Journal of Earth Sciences》2014,103(3):843-875

The Monte Ascensione succession (c. 2.65–2.1 Ma) is a well-exposed example of an exhumed submarine canyon fill embedded within slope hemipelagic mudstones. This gorge represented a long-lasting pathway for sediment transport and deposition and during the Gelasian delivered Apennine-derived clastic sediment to the adjacent Peri-Adriatic basin. A total of six principal lithofacies types, representing both canyon-confining hemipelagic deposits and canyon-filling turbidity current and mass-transport deposits, can be delineated in the studied sedimentary succession. The canyon-fill deposits display a marked cyclic character and the component lithofacies succeed one another to form at least fifteen fining-upward stratal units, which are interpreted to represent high-frequency, unconformity-bounded depositional sequences. Variability in the vertical repetition of constituent lithofacies allows the identification of three basic styles of sequence architecture that can be interpreted in terms of differing positions along a conceptual down-canyon depositional profile. An integrated chronology, based on biostratigraphic data and on palaeomagnetic polarity measurements, strongly supports a one-to-one correlation between the sequence-bounding surfaces and oxygen isotope stages G2–78, suggesting that the most feasible sequence-engendering mechanism is that of orbitally dictated glacio-eustatic changes in sea level, which regulated timing of sediment storage on the shelf and its redistribution beyond the shelf edge. One of the most significant aspects of this study is the demonstration that processes occurring within upper slope canyons can be expected to be strongly influenced by variations in sea level; that is, the erosional and depositional features evident in these deposits can be strongly controlled by allocyclic processes rather than autocyclic or random processes.  相似文献   

The Rosetta Marbles from Fesleğen, Ören Unit,SW Anatolia     

Franziska Scheffler  Roland Oberhänsli  Amaury Pourteau  Osman Candan  Matteo Di Lucia 《International Journal of Earth Sciences》2014,103(2):485-486

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The volcanic and geothermally active Campi Flegrei caldera: an integrated multidisciplinary image of its buried structure     

M. Piochi  C. R. J. Kilburn  M. A. Di Vito  A. Mormone  A. Tramelli  C. Troise  G. De Natale 《International Journal of Earth Sciences》2014,103(2):401-421

The Campi Flegrei caldera in southern Italy is one of the greatest geohazard areas on Earth. Evidence of an active magmatic and geothermal system is provided by ongoing ground uplift, with volcano-tectonic and long-period (LP) seismicity, the persistent degassing of ~1500 tonnes of CO₂ per day, the presence of hot fumaroles at temperatures of 90–150 °C, brine-rich aquifers (with total dissolved solids up to 33 g l^?1) and high thermal gradients in the crust (with temperatures reaching 420 °C at 3,050 m b.s.l.). Since the 1940s, more than 100 exploratory boreholes have been drilled in the area to depths of 80–3,100 m by the Azienda Geologica Italiana Petroli (AGIP) and the Società Anonima Forze Endogene Napoletane (SAFEN). To date, however, no systematic reanalysis of the drilling data has been carried out, and the buried volcanic structure has not been updated using the most recent scientific results and previous findings. By integrating unpublished data from the AGIP and SAFEN reports with published information from geological, volcanological, petrological, petrophysical and geophysical studies, this paper presents an improved picture of the Campi Flegrei caldera that will be useful for volcanic hazard assessment and mitigation in the Naples area and for future research planning. The results suggest that intra-caldera activity has been influenced by how the magmatic system at depths greater than about 4 km has determined the transfer of magma, volatiles, and heat to the overlying geothermal system and, ultimately, to the surface. In particular, intriguing is that the most volcanically active central-eastern sector of the caldera, which is subject to intense bradyseismic ground movement and gas emission, coincides with a structurally delimited subsurface rock volume characterized by an uprising of the 100 °C isotherm, a deep water supply to the shallower aquifer, the early disappearance of secondary calcite, LP seismicity and high seismic S-wave attenuation. In this area, we also document evidence of repeated injection at depths of c. 1.5–3.0 km of isolated and small-volume batches of magma, where occurred their crystallization and degassing. Shallow intrusions and degassing of magma are thus identified as two of the key processes that drive unrest in Campi Flegrei.  相似文献   

巴布亚新几内亚铜金矿床成矿时代及成矿控制因素     

宋学信  信迪  王天刚  隋鑫  景丽姿  杨艳 《地质通报》2014,(Z1):283-298

巴布亚新几内亚是在澳大利亚板块与太平洋板块斜向和快速汇聚的边界带内演化的,是世界上构造运动最复杂的区带之一,其地球动力学演化涉及俯冲与火山岛弧(岩浆弧)形成、弧陆碰撞与造山、俯冲陆壳折返—岩浆侵入—成矿作用等地质作用。地质年代学研究指出,巴布亚新几内亚主岛(新几内亚岛)的地球动力学次序是:①引起抬升和折返的碰撞作用;②折返期间或稍后的侵入作用;③侵入岩体系晚期的成矿事件。在地球动力学次序中,巴布亚新几内亚铜金成矿时代主要集中在25~0Ma之间,其中几个世界级矿床更为年轻,成矿年龄只有6~0Ma。笔者按成矿时代将巴布亚新几内亚铜金成矿作用分为第一高潮(23~12Ma)、第二高潮(7~1Ma)和第三高潮(现在进行时)(0.5~0Ma)。巴布亚新几内亚铜金成矿受大地构造、侵入杂岩体、特定赋矿地层、转换构造、背斜、各种断裂、破火山或火山管道等控制。  相似文献   

大洋洲地区矿产地数据库建设     

陈刚  姚仲友  王天刚  高卫华  孔红杰  信迪 《地质通报》2014,(Z1):164-171

依据数据库建库标准、建库流程、数据质量控制措施等方法和流程,构建了大洋洲地区铁、锰、铜、铝、金、镍、铀、稀土元素矿产地数据库。通过对矿产地数据特征与地学多源信息的综合分析,总结区域成矿规律,提供了矿产资源预测的基础数据。形成的数据库管理系统对资料管理、查询、利用更方便,表达更直观,分析和总结更有效。  相似文献   

新西兰海潮负荷位移建模精度分析     

刘中冠  袁林果  陈昌福  成帅  张迪 《大地测量与地球动力学》2021,41(4):387-391

为评价新西兰海潮负荷位移建模精度,利用新西兰189个GPS站11 a的实测数据,基于静态精密单点定位测定8个半日潮波及周日潮波的海潮负荷位移参数,并将其与7种全球海潮模型及4种地球模型计算的海潮负荷位移改正值进行比较。结果表明：1）TPXO7.2模型负荷位移改正值与GPS解算的海潮负荷位移参数最符合,M2、N2、O1和Q1潮波均方根误差在水平方向小于0.5 mm,垂直方向小于0.7 mm;2）不同地球模型对确定海潮负荷位移的影响主要体现在M2和N2潮波;3）GPS估值和海潮模型值之间的残差矢量呈现出大小及方向上的区域一致性,部分站点异常的残差值可能反映出当前SNREI地球模型的缺陷。  相似文献   

高淀粉水平下精氨酸对松浦镜鲤肠道形态与功能的影响     

李晋南  王常安  张圆圆  吴迪  范泽  王连生 《广东海洋大学学报》2021,(1)

【目的】探讨高淀粉饲料中添加精氨酸对松浦镜鲤(CyprinuscarpioL.)肠道消化酶活性及肠道形态的影响。【方法】选用初始体质量(6.84±0.02)g的松浦镜鲤360尾,随机分为5组,每组4个重复,每个重复18尾鱼。实验饲料分为5组,分别在45%水平的高淀粉饲料中添加质量分数0%、0.6%、1.2%、1.8%、2.4%的精氨酸,实验周期为8周,进行肠道消化酶和形态的测定。【结果】前、中、后肠的淀粉酶活性,各组之间没有显著差异(P> 0.05);添加2.4%精氨酸组的前肠脂肪酶活性显著高于对照组(P <0.05),中肠和后肠的脂肪酶活性各组间没有显著差异(P>0.05);前、中、后肠蛋白酶活性随精氨酸添加量的增加而增加,添加1.8%和2.4%精氨酸组的前肠和中肠蛋白酶活性显著高于对照组(P<0.05),添加2.4%精氨酸组后肠的蛋白酶活性显著高于对照组(P<0.05)。高淀粉饲料中添加Arg显著影响了肠道皱襞高度,但对肠绒毛宽度和肌层厚度没有显著影响。2.4%精氨酸组前肠皱襞高度显著高于其他各组(P <0.05),1.8%精氨酸组中肠和后肠皱襞高度显著高于对照组(P <0.05)。1.2%、1.8%和2.4%组肠体指数显著高于对照组(P <0.05),2.4%精氨酸组肠长指数显著高于对照组(P <0.05)。各组前、中、后肠肠绒毛密度没有显著差异,且排列较整齐。【结论】高淀粉饲料中添加1.8%~2.4%精氨酸可以增加松浦镜鲤肠道消化酶活性,同时改善了松浦镜鲤的肠道形态结构。  相似文献   

河套地区典型干线的形成及其在对流触发中的作用     

张一平  俞小鼎  王迪  郝晓珍  王金兰 《气象学报》2022,80(1):39-53

利用高空、加密地面、EC-ERA5(0.25o×0.25o)再分析和FY-2系列静止气象卫星云图(可见光星下点分辨率1.25 km,红外5 km)等资料,对黄河河套地区3次典型干线的形成及其在对流触发中的作用进行了详细分析.结果表明:(1)3次干线触发对流出现在中高纬度高空槽东移诱发蒙古气旋发展的背景下,高低空系统配置...  相似文献   

基础测绘转型升级融入自然资源管理的思考     

吴迪  汪建光 《地理空间信息》2022,20(4):44-47,146

在自然资源管理机构改革的大背景下,围绕浙江省基础测绘工作运行的实际情况,分析了浙江省基础测绘融入自然资源管理体系的现状和存在的问题.就如何提升基础测绘支撑职责"两统一"管理能力,提出了构建多种适应新形势的统筹机制,以保障基础测绘各项工作向纵深开展、优化产品形式和产品的更新频率,提升基础测绘服务水平和服务能力、提升技术水...  相似文献   

Adsorption behaviors of Cd^2＋ on Fe2O3/MnO2 and the effects of coexisting ions under alkaline conditions   总被引：2，自引：0，他引：2  

Zuwei Wang  Xiangfeng Zeng  Xiaoman Yu  Hui Zhang  Zhaojiang Li  Di Jin 《中国地球化学学报》2010,29(2):197-203

This study describes the adsorption features of cadmium on Fe2O3 and MnO2 in alkaline saline conditions. The adsorption reached equilibrium in 6 hours under alkaline conditions. The absorption of cadmium on Fe2O3 and MnO2 was consistent with Freundlich absorption isotherms, and the corresponding adsorption capacities were 16.3 and 16.7 mg·g-1, respectively. Moreover, the adsorption quantity of cadmium on Fe2O3 and MnO2 rose with increasing pH from acidic to neutral, and reached the maximum at pH= 9. The coexisting chlorides reduced the adsorption capacity of Fe2O3 and MnO2. The influence intensities of different cations follow the order of CaCl2>>KCl>NaCl. However, the influence of sodium salts on the capacities of Fe2O3 and MnO2 to adsorb cadmium appeared more complicated: the relatively low concentrations of sodium salts could reduce the adsorption capacity; with increasing concentrations of sodium salts, e.g. NaCl and NaNO3. The adsorption capacity decreased continually. Moreover, due to the competition adsorption and precipitation effects, the adsorption capabilities of Na2CO3, NaH2PO4 and Na2HSO4 could also be reduced and cadmium concentrations in the solution were reduced as well.  相似文献