Magma Chamber Process of Post-collisional Magmatism: Insight from Textural and Elemental Characteristics of Plagioclase from the Tatun Volcanic Group, Northern Taiwan Volcanic Zone     

ZHANG Xi  GUO Kun  ZHANG Yu  LAI Zhiqing  JIANG Shulong  JIANG Wenpeng  LI Jingbo 《《地质学报》英文版》2022,96(5):1587-1599

The Taiwan mountain belt, one of the youngest orogenies in the world, is caused by the collision of the Luzon arc with the Eurasian margin, which leads to post-collisional extension and magmatism in the Northern Taiwan Volcanic Zone (NTVZ). The magma chamber process in this region has not previously been elucidated in detail. In this paper, the textural and compositional features of plagioclase phenocrysts in basalt from the Tatun Volcanic Group (TTVG) were studied to restrict the dynamics of magma system. Results show that the magma melts in TTVG are mainly sourced from the underlying MORB-like mantle wedge but influenced by incorporation of subduction components, causing the elevated Sr/Y and Ba/Y ratios in magma melts. The subduction components are mainly transported in the form of sediment melt. The plagioclase phenocrysts in the TTVG volcanic rocks are generally coarsely core-sieved with a clear rim. The An contents in the rims of plagioclase are much lower than those of cores, and elevated FeO concentrations are detected in the plagioclase rims. We propose there exists a double-layer magma chamber in this region. The core of the plagioclase was crystalized in the deeper quiescent magma chamber (~21 km), which was subsequently partially dissolved during the ascent of magma melt under H2O-undersaturated condition, forming the typical coarsely sieved texture and synneusis. When this crystal-rich melt migrates into the shallower chamber, water saturation is reached and more sodic plagioclase formed as the rim of phenocryst. Due to the considerably higher fO2 in the shallow chamber than in the deeper one, and the distribution of Fe between plagioclase and melt positively correlates with fO2, the FeO content in the plagioclase rim elevates in conjunction with increasing fO2.  相似文献   

竖向入射S波作用下单桩水平地震响应简化解析方法     

郑长杰  崔亦秦  吴琛  罗通  栾鲁宝 《岩土力学》2023,(2):327-336

基于连续介质模型并考虑桩-土运动相互作用,将单桩视为一维线弹性梁,研究了竖向入射S波作用下的单桩水平地震响应问题。将竖向入射S波模拟为基岩水平位移,基于平面应变模型建立的土体控制方程,推导出地震作用下土体水平动力阻抗函数表达式。将土体阻抗代入单桩控制方程并联立桩-土接触条件及桩顶和桩底的边界条件,得出了竖向入射S波作用下单桩的地震响应解析解。通过将所得解与已有文献理论解和有限元结果进行对比,验证了该方法的合理性。基于所得理论解进行参数分析得出：桩-土模量比的增加可以明显降低桩-土运动相互作用因子的最小值,而较大桩身长径比以及土体滞回阻尼对桩-土运动相互作用因子的影响较小;对于桩顶水平地震放大因子来说,桩-土模量比的增加仅在高共振频率处抑制其幅值,较大桩身长径比对其影响较小,而滞回阻尼比的增加会显著抑制共振频率处的幅值;桩身地震响应仅在较小桩径比时受桩-土模量比的影响明显,并随桩-土模量比的增加而降低。  相似文献   

祁连山地区生态系统服务间权衡的社会-生态环境响应机制研究   总被引：1，自引：0，他引：1  

吕荣芳  赵文鹏  田晓磊  张建明 《冰川冻土》2021,43(3):928-938

生态系统服务间权衡和协同关系存在显著的空间异质性,现有研究较少从社会-生态环境的角度进行分析,难以对将生态系统服务纳入实际政策制定过程中。以祁连山地区为研究区,利用InVEST模型和CASA模型对2019年五项调节服务（碳固定、碳储存、产水量、土壤保持和水质净化）和一项支持服务（生境质量）进行计算,结合多元回归树分析法,研究服务间关联的空间异质性及其对社会-生态环境的响应。结果显示,全区尺度上六项服务间呈协同关系,主要受到土地利用类型、降雨和植被覆盖度的影响。植被覆盖区的服务供给量整体高于无植被覆盖区。研究区可被分为5个聚类,不同聚类内服务间关联存在差异。无植被覆盖且年均降雨量低于440.2 mm的区域与植被覆盖度高于0.559的非耕地区内,服务间关联均呈显著协同,后者服务整体较高。降雨升高可促使无植被覆盖区内产水量和土壤保持与其他服务间呈权衡关系,植被覆盖度较低或耕地区内服务间关联变弱。研究成果可为生态管理和政策制定提供有效参考。  相似文献   

海河流域地下水资源特征和开发利用潜力          下载免费PDF全文

杨会峰  孟瑞芳  李文鹏  李泽岩  支传顺  包锡麟  李长青  柳富田  吴海平  任宇 《中国地质》2021,48(4):1032-1051

海河流域水资源严重短缺,地下水长期超采是制约社会经济可持续发展的主要瓶颈。开展流域地下水资源及开发利用潜力研究,对支撑服务地下水超采治理、地下水资源可持续利用和生态环境保护都具有重要意义。经系统评价,海河流域天然资源量252.99×10~8m~3,生态水位约束条件下的浅层地下水开采资源量172.98×10~8m~3,可更新的深层水可利用量4.68×10~8m~3。海河流域山区地下水质量总体较好,Ⅰ～Ⅲ类水占比40.83%,平原区浅层地下水质量较差,Ⅰ～Ⅲ类水占比14.10%,深层地下水质量优于浅层地下水,Ⅰ～Ⅳ类水占比74.25%。海河流域山区地下水开采潜力总体较小,燕山和太行山北部山区,地下水资源禀赋较差,基本无开采潜力,太行中部山区地下水开采程度较高,无开采潜力或开采潜力较小,太行南部山区地下水资源禀赋良好,开采潜力较大;平原区浅层地下水在不同水文地质单元开采潜力差异较大,山前平原浅层地下水长期超采形成大范围降落漏斗,无开采潜力或潜力较小,中东部平原浅层地下水资源禀赋较差,以微咸水为主,开采潜力较小,山东省鲁北平原区浅层地下水开采程度较低,聊城—德州一带开采潜力较大;雄安新区地下水总体无开采潜力。平原区深层地下水基本无开采潜力。  相似文献   

甘肃省2000-2009年碳循环研究     

肖玲  赵先贵  栾建伟 《地域研究与开发》2012,31(5)

对甘肃省2000-2009年的碳源和碳汇进行了研究,获得了该地区碳源、碳汇随时间变化的预测模型,并预测了未来的发展趋势.结果表明,甘肃省碳源由2000年的4.294 7×108 t/a逐年增加至2009年的5.6307×108t/a,10年间增加了31.11％.而同期碳汇由3.9595×108t/a逐年增加到4.8991×108t/a,仅增加了23.73％.显然,碳源的增加速率高于碳汇.甘肃省2000年碳失汇为0.3352×108t/a,2009年增至0.7316×108 t/a.预测甘肃省2015年碳源总量将达到6.7193×108t/a,碳汇总量为5.5487×108 t/a,碳失汇将达到1.1706×108t/a.显而易见,如不改变现有的发展模式,甘肃碳源与碳汇的失衡将不断加剧,碳安全面临更严峻的考验.  相似文献   

中国东北红河国家级自然保护区湿地植被空间格局与环境梯度关系(英文)   总被引：1，自引：0，他引：1  

周德民  栾兆擎  郭逍宇  娄彦景 《地理学报(英文版)》2012,22(1):57-70

Quantifying correlation between the spatial patterns of natural wetland plants and environmental gradient gives better understanding of wetland habitats, which is the fundamental for the strategy making on the protection and restoration of natural wetlands. In this study, the spatial patterns of wetland plants and the environmental gradient of wetland habitats were assessed in the Honghe National Nature Reserve (HNNR) in Northeast China, a wetland of international importance on the Ramsar list. Biophysical parameters’ values of wetland plants were obtained by field sampling methods, and wetland mapping at the community scale was completed using remote sensing techniques. Digital delineation of the surface water system, hydrological zoning and wetness index were produced by spatial analysis methods in Geographic Information System. An ecological ordination method and two clustering methods were used to quantify the relationship between the spatial distribution patterns of wetland plants and the corresponding environmental gradients. Such quantitative analyses also present the specific diversity of different types of wetland plants based on the environmental attributes of their habitats. With the support from modern geo-information techniques, the experimental results indicate how four ecotypes of wetland plants spatially transit from forest swamp, shrub wetland and meadow into marsh wetland with increasing wetness index and water table. And they also show how wetland spatial distribution patterns are controlled by an environmental gradient of wetness. Another key finding of this research work is that our results present the exact fundamental differences between marsh and non-marsh plants of 11 wetland plant communities within the core study area. Hence, this case study gives a good sample for better understanding of the complex correlation between the spatial patterns of wetland plants and their environmental attributes using advanced digital analysis methods. It is also useful to show how to integrate geoinformatic techniques with statistical analysis methods based on the field data base.  相似文献   

济南市CO中毒的天气形势分析     

栾怀德  刘洪鹏  李华 《山东气象》2008,28(2)

利用2001-2003年济南市的CO中毒资料及同期高空、地面天气图,统计了CO中毒日的月、季变化特征,分析CO中毒事件所对应的天气形势背景,总结出8种高空风场和温度场的配置类型,在此基础上重点分析了各种类型所对应的地面气压场,结果表明:济南市采暖季节,CO中毒事件多发生在地面为南高北低、东高西低和维持时间较长的均压场和鞍型场的气压场中.风向、风速、气温、湿度等气象要素与CO中毒事件的发生有着一定的对应关系.  相似文献   

Local-scale spatial variability of soil organic carbon and its stock in the hilly area of the Loess Plateau, China   总被引：3，自引：0，他引：3  

Yafeng Wang  Yihe Lü  Yong Luan 《Quaternary Research》2010,73(1):70-76

Soil organic carbon (SOC) is one of the key components for assessing soil quality. Meanwhile, the changes in the stocks SOC may have large potential impact on global climate. It is increasingly important to estimate the SOC stock precisely and to investigate its variability. In this study, Yangjuangou watershed was selected to investigate the SOC distribution under different land uses. We found that SOC concentration decreased with increasing soil depth under all land uses and was significantly different across the vertical soil profile (P < 0.01). However, considering effect of land use on SOC, it is only significant (P < 0.01) in the topsoil (0-5 cm) layer. This indicated that land use has a large effect on the stocks of SOC in the surface soil. The stratification ratio of SOC > 1.2 may mean that soil quality is improving. The order of the SOC density (0-30 cm) under different land uses is forestland > orchard land > grassland > immature forestland > terraced cropland. The SOC stock is found to be as large as 2.67 × 10³ t (0-30 cm) in this watershed. Considering time effect of restoration, the slope cropland just abandoned is more efficient for SOC accumulation than trees planted in the semi-arid hilly loess area.  相似文献   

Activity and Formation of Sand Waves on Northern South China Sea Shelf     

栾锡武  彭学超  王英民  邱燕 《中国地质大学学报(英文版)》2010,(1)

Sand waves on the northern South China Sea shelf had been considered as stable relict bed form. For the industry use of sea bed between stations LF13-2 and LF13-1, a new round of explorations were conducted. The newly obtained data show that both spacings and amplitudes of sand waves are all systematically changing with water depth. Repeated observations since 2003 to 2004 showed that the sea bed is currently active. Due to strong erosion of surface sediment since Dongsha (东沙) uplifting, there are almost no...  相似文献   

丹宁棉分离富集—发射光谱法同时测定地质样品中微量铌钽锆铪   总被引：1，自引：1，他引：1  

李滦宁  马玖彤等 《岩矿测试》2001,20(1):27-30

采用丹宁棉对地质样品溶液中的铌、钽、锆、铪进行分离富集，将写信后的丹宁棉在600℃灼烧30min，灰分用发射光谱法同时测定四元素。检出限与通常的发射光谱法相比降低约2个数量级，经国家级标准物质检验，结果与标准值相符，精密度试验，各元素的RSD（n＝20）为2.6％－7.9％。  相似文献