Objective The Qinling Mountains （QM） in Central China is a natural harrier that corresponds to the boundary between the southern and northern climate and environment （Gong Hujun et al., 2017）. Northern QM is rela...Objective The Qinling Mountains （QM） in Central China is a natural harrier that corresponds to the boundary between the southern and northern climate and environment （Gong Hujun et al., 2017）. Northern QM is relatively steep, and southern QM is in contrast relatively low and gentle. Investigations have shown that the average uplift rate of northern QM since 17.8 Ma is approximately 0.19 mm/a （Yin Gongming et al., 2001）, whereas that of central QM since 0.36 Ma is approximately 0.32 mm/a （Wang Fei et al., 2004）. To date, however, few investigations have yet been conducted on the uplift rate of southern QM. Accordingly, we aim to obtain the uplift rate of southern QM by using the cosmogenic ^26A1/^10 Be burial dating method to determine the age of the highest river terrace on the southern slope of QM.展开更多
Jinlongshan gold orebelt, a newly discovered one in sedimentary rock region in southern Qinling Mountains, is mainly located in upper Devonian and lower Carboniferous calcareous siltstone and argillic silty limestone ...Jinlongshan gold orebelt, a newly discovered one in sedimentary rock region in southern Qinling Mountains, is mainly located in upper Devonian and lower Carboniferous calcareous siltstone and argillic silty limestone of later Paleozoic era. Typical disseminated gold mineralization occurred in calcareous siltstone, which is major host rock and mainly composed of silt (SiO2 mostly varies from 38% to 73%) and calcite (CaO mostly varies from 10% to 25%). Pyrite created by living beings in Nanyangshan formation may be poor in gold. Faults and favorable layers jointly control disseminated gold mineralization. The significance of this opinion is very great for gold exploration.展开更多
秦岭北麓地区地势复杂、气候多变,生态环境丰富多样,是中国独特的生态宝库之一。而随着经济发展和人口增加,其生态环境也面临着严峻的挑战,保护其生态环境已成为当前亟待解决的问题。为此,该研究提出了一种结合“驱动力-压力-状态-影响...秦岭北麓地区地势复杂、气候多变,生态环境丰富多样,是中国独特的生态宝库之一。而随着经济发展和人口增加,其生态环境也面临着严峻的挑战,保护其生态环境已成为当前亟待解决的问题。为此,该研究提出了一种结合“驱动力-压力-状态-影响-响应-管理”(driving-force-pressure-state-impact-response-management,DPSIRM)和斑块生成土地利用变化模拟(patch-generating land use simulation,PLUS)模型来评价秦岭北麓生态环境的方法。首先,基于DPSIRM模型,选取了17个指标对2010、2015、2020年的秦岭北麓生态环境状况进行生态敏感性评价,其次在此基础上运用PLUS模型预测不同情景下2020–2030年秦岭北麓土地利用空间布局情况,最后利用预测的土地利用类型数据作为影响生态环境的因子,预测研究区的生态敏感性空间分布特征。结果表明:秦岭北麓生态敏感区主要分布在中心城区周围,距城区越远,抗干扰能力越强;2010–2020年非敏感性区域逐步增多,从9%增加到了26%,2010年低敏感区占比最多(38%),2015年中敏感区占比最多(28%),2020年低敏感区占比最多(30%),极高敏感区整体占比不高且相差不大(5%~10%),表明随着时间的变化研究区生态环境已得到初步改善且总体状态向好发展;2020–2030年3种不同情景下土地利用类型主要以耕地、林地、草地为主,模拟预测发现以生态保护为前提的保护与开发是较为适应当前可持续发展战略的情景。研究结果可为研究区生态环境保护和可持续土地利用提供科学依据。展开更多
基金supported by the National Natural Science Foundation of China(grants No.41572155 and 41690111)the Global Change Program of the Ministry of Science and Technology of China(grant No.2016YFA0600503)
文摘Objective The Qinling Mountains （QM） in Central China is a natural harrier that corresponds to the boundary between the southern and northern climate and environment （Gong Hujun et al., 2017）. Northern QM is relatively steep, and southern QM is in contrast relatively low and gentle. Investigations have shown that the average uplift rate of northern QM since 17.8 Ma is approximately 0.19 mm/a （Yin Gongming et al., 2001）, whereas that of central QM since 0.36 Ma is approximately 0.32 mm/a （Wang Fei et al., 2004）. To date, however, few investigations have yet been conducted on the uplift rate of southern QM. Accordingly, we aim to obtain the uplift rate of southern QM by using the cosmogenic ^26A1/^10 Be burial dating method to determine the age of the highest river terrace on the southern slope of QM.
文摘Jinlongshan gold orebelt, a newly discovered one in sedimentary rock region in southern Qinling Mountains, is mainly located in upper Devonian and lower Carboniferous calcareous siltstone and argillic silty limestone of later Paleozoic era. Typical disseminated gold mineralization occurred in calcareous siltstone, which is major host rock and mainly composed of silt (SiO2 mostly varies from 38% to 73%) and calcite (CaO mostly varies from 10% to 25%). Pyrite created by living beings in Nanyangshan formation may be poor in gold. Faults and favorable layers jointly control disseminated gold mineralization. The significance of this opinion is very great for gold exploration.
文摘秦岭北麓地区地势复杂、气候多变,生态环境丰富多样,是中国独特的生态宝库之一。而随着经济发展和人口增加,其生态环境也面临着严峻的挑战,保护其生态环境已成为当前亟待解决的问题。为此,该研究提出了一种结合“驱动力-压力-状态-影响-响应-管理”(driving-force-pressure-state-impact-response-management,DPSIRM)和斑块生成土地利用变化模拟(patch-generating land use simulation,PLUS)模型来评价秦岭北麓生态环境的方法。首先,基于DPSIRM模型,选取了17个指标对2010、2015、2020年的秦岭北麓生态环境状况进行生态敏感性评价,其次在此基础上运用PLUS模型预测不同情景下2020–2030年秦岭北麓土地利用空间布局情况,最后利用预测的土地利用类型数据作为影响生态环境的因子,预测研究区的生态敏感性空间分布特征。结果表明:秦岭北麓生态敏感区主要分布在中心城区周围,距城区越远,抗干扰能力越强;2010–2020年非敏感性区域逐步增多,从9%增加到了26%,2010年低敏感区占比最多(38%),2015年中敏感区占比最多(28%),2020年低敏感区占比最多(30%),极高敏感区整体占比不高且相差不大(5%~10%),表明随着时间的变化研究区生态环境已得到初步改善且总体状态向好发展;2020–2030年3种不同情景下土地利用类型主要以耕地、林地、草地为主,模拟预测发现以生态保护为前提的保护与开发是较为适应当前可持续发展战略的情景。研究结果可为研究区生态环境保护和可持续土地利用提供科学依据。
