On the basis of the relationship between tree ring width of Pinus tabulaeformis in the southern Taihang Mountains in Hebei Province and climate factors, such as mean temperature, mean maximum temperature, mean minimum...On the basis of the relationship between tree ring width of Pinus tabulaeformis in the southern Taihang Mountains in Hebei Province and climate factors, such as mean temperature, mean maximum temperature, mean minimum temperature and precipitation, we find that tree-ring width correlates positively and significantly with mean and maximum temperature in March and Spring, and with minimum temperature in March, April, Spring and Autumn. The sampling tree radial growth responds sensitively to spring temperature change.展开更多
The relationships between the normalized difference vegetation index(NDVI)(1981-2006) in growing season and precipitation, NDVI and mean temperature(T_(mean)), NDVI and maximum temperature(T_(max)), NDVI and minimum t...The relationships between the normalized difference vegetation index(NDVI)(1981-2006) in growing season and precipitation, NDVI and mean temperature(T_(mean)), NDVI and maximum temperature(T_(max)), NDVI and minimum temperature(T_(min)), and NDVI and the Palmer Drought Severity Index(PDSI) were analyzed. The results indicated that NDVI during the growing season was mostly positively and significantly correlated with precipitation last month and the month before last, and mostly negatively with temperature. There were negative and significant correlation between NDVI in June and July and T_(mean)and T_(max)in May respectively, between April NDVI and T_(min)in February and March, and between June NDVI and T_(min)in April, May and June. Vegetation cover in growing season correlated positively with PDSI, especially those last month and the month before last at 0.05 significance level, even 0.01 level. Hydrothermal conditions from March to July had significant influence on vegetation cover.展开更多
The late Cenozoic geomorphic features and geochronologic data of the Zhingfang River catchment in the Yuntaishan World Geopark are studied. Several quarternary geochronologic methods, including electron spin resonance...The late Cenozoic geomorphic features and geochronologic data of the Zhingfang River catchment in the Yuntaishan World Geopark are studied. Several quarternary geochronologic methods, including electron spin resonance （ESR）, optically stimulated luminescence （OSL）, thermo-luminescence （TL） and U-series are presented in this paper. The results suggest that there are two planation surfaces, named as the Taihang surface which is a peneplain of Taihang stage formed during Oligocene or Oligocene to early-middle Miocene period, and Tang-hien surface which is a mature wide valley of Tang-hien stage formed during late Miocene-Pliocene or Piiocene-early Pleistocene period and probably ended prior to 2.2-2.6 Ma based on ESR dating. After the Tang-hien stage, the incision and aggradation of the river formed six stream terraces with heights of 3-5 m, 8-12 m, 22-24 m, 28-38 m, 50-62 m and 80-85 m above the river bottom, respectively. The dating results of the alluvium sediments suggest that these terraces were formed during Holocene, 20-23 ka B.P., 110-120 ka B.P., 200-240 ka B.P., 840-1200 ka B.P. or ~450 ka B.P. and 1600-1800 ka B.P. or -1100 ka B.P., respectively. These results indicate that episodic incision of the river, which controls the formation of the scenery in the Yuntaishan World Geopark, was mainly influenced by the periodic dry-wet climate change during late Cenozoic mountain uplift.展开更多
长城系是华北克拉通统一结晶基底形成后的首套沉积盖层,其碎屑锆石U-Pb年代学及其Hf同位素特征分析对探讨地层形成时代、源区特征以及基底演化均具重要研究意义。本文对华北克拉通中部黎城地区长城系下部地层的碎屑锆石进行了U-Pb年龄...长城系是华北克拉通统一结晶基底形成后的首套沉积盖层,其碎屑锆石U-Pb年代学及其Hf同位素特征分析对探讨地层形成时代、源区特征以及基底演化均具重要研究意义。本文对华北克拉通中部黎城地区长城系下部地层的碎屑锆石进行了U-Pb年龄和Hf同位素分析。结果表明,该区长城系碎屑锆石U-Pb年龄呈现了2.55~2.45Ga、2.15~2.0Ga和~1.92Ga等三个主峰期,同时存在3.5~3.1Ga和2.9~2.7Ga的年龄次峰期。最年轻碎屑锆石的207 Pb/206 Pb加权平均年龄限定了该区长城系沉积发生于1.76Ga之后。碎屑锆石的年龄分布和Hf同位素特征与华北克拉通中、南部基底物质记录的地质事件高度相似,区内长城系地层与南部熊耳地区长城系地层可对比性强,证明太行山南段在1.76Ga后已与南部熊耳裂谷盆地相连,其沉积物质均主要来自华北克拉通中、南部地区。其中,3.5~3.4Ga的古老碎屑锆石εHf(t)=-8.6~-4.6,揭示中、南部地区存在古太古代地壳物质。新太古代早期2.9~2.7Ga的锆石εHf(t)以正值为主(占比85%),它们的t C DM=3190~2774Ma,与其结晶年龄相同或接近,证明华北克拉通南部在新太古代早期以新生地壳生长为主。新太古代晚期2.55~2.45Ga峰期的锆石也以正的εHf(t)值为主(占比69%),而2.15~2.0Ga峰期锆石的εHf(t)值大多偏负(占比56%),说明华北克拉通南部地区从新太古代末期的新生地壳增生为主伴有陆壳再造转变为古元古代中期以古老陆壳物质再造为主,并有少量新生陆壳增生;古元古代晚期~1.92Ga年龄峰期的碎屑锆石εHf(t)=-11.9~+2.0,揭示至古元古代末期华北克拉通中南部进入到以古老陆壳物质再造为主的演化阶段。展开更多
基金Supported by the Science and Technology Plan Projects of Hebei Province(15454201D)
文摘On the basis of the relationship between tree ring width of Pinus tabulaeformis in the southern Taihang Mountains in Hebei Province and climate factors, such as mean temperature, mean maximum temperature, mean minimum temperature and precipitation, we find that tree-ring width correlates positively and significantly with mean and maximum temperature in March and Spring, and with minimum temperature in March, April, Spring and Autumn. The sampling tree radial growth responds sensitively to spring temperature change.
基金Supported by the Science and Technology Plan Projects of Hebei Province(15454201D)
文摘The relationships between the normalized difference vegetation index(NDVI)(1981-2006) in growing season and precipitation, NDVI and mean temperature(T_(mean)), NDVI and maximum temperature(T_(max)), NDVI and minimum temperature(T_(min)), and NDVI and the Palmer Drought Severity Index(PDSI) were analyzed. The results indicated that NDVI during the growing season was mostly positively and significantly correlated with precipitation last month and the month before last, and mostly negatively with temperature. There were negative and significant correlation between NDVI in June and July and T_(mean)and T_(max)in May respectively, between April NDVI and T_(min)in February and March, and between June NDVI and T_(min)in April, May and June. Vegetation cover in growing season correlated positively with PDSI, especially those last month and the month before last at 0.05 significance level, even 0.01 level. Hydrothermal conditions from March to July had significant influence on vegetation cover.
基金the work of "Study of the geo-scientific settings of geo-tourist landscapes in Yuntaishan World Geopark",and supported by the Department of International Cooperation of Ministry of Science and Technology of China. (Grant No. 2006DFA21320)the Science Foundation of institute of geomechanics, CAGS (Grant No. DZLXJK200706) the National Natural Science Foundation of China (Grant No. 40501006)
文摘The late Cenozoic geomorphic features and geochronologic data of the Zhingfang River catchment in the Yuntaishan World Geopark are studied. Several quarternary geochronologic methods, including electron spin resonance （ESR）, optically stimulated luminescence （OSL）, thermo-luminescence （TL） and U-series are presented in this paper. The results suggest that there are two planation surfaces, named as the Taihang surface which is a peneplain of Taihang stage formed during Oligocene or Oligocene to early-middle Miocene period, and Tang-hien surface which is a mature wide valley of Tang-hien stage formed during late Miocene-Pliocene or Piiocene-early Pleistocene period and probably ended prior to 2.2-2.6 Ma based on ESR dating. After the Tang-hien stage, the incision and aggradation of the river formed six stream terraces with heights of 3-5 m, 8-12 m, 22-24 m, 28-38 m, 50-62 m and 80-85 m above the river bottom, respectively. The dating results of the alluvium sediments suggest that these terraces were formed during Holocene, 20-23 ka B.P., 110-120 ka B.P., 200-240 ka B.P., 840-1200 ka B.P. or ~450 ka B.P. and 1600-1800 ka B.P. or -1100 ka B.P., respectively. These results indicate that episodic incision of the river, which controls the formation of the scenery in the Yuntaishan World Geopark, was mainly influenced by the periodic dry-wet climate change during late Cenozoic mountain uplift.
文摘长城系是华北克拉通统一结晶基底形成后的首套沉积盖层,其碎屑锆石U-Pb年代学及其Hf同位素特征分析对探讨地层形成时代、源区特征以及基底演化均具重要研究意义。本文对华北克拉通中部黎城地区长城系下部地层的碎屑锆石进行了U-Pb年龄和Hf同位素分析。结果表明,该区长城系碎屑锆石U-Pb年龄呈现了2.55~2.45Ga、2.15~2.0Ga和~1.92Ga等三个主峰期,同时存在3.5~3.1Ga和2.9~2.7Ga的年龄次峰期。最年轻碎屑锆石的207 Pb/206 Pb加权平均年龄限定了该区长城系沉积发生于1.76Ga之后。碎屑锆石的年龄分布和Hf同位素特征与华北克拉通中、南部基底物质记录的地质事件高度相似,区内长城系地层与南部熊耳地区长城系地层可对比性强,证明太行山南段在1.76Ga后已与南部熊耳裂谷盆地相连,其沉积物质均主要来自华北克拉通中、南部地区。其中,3.5~3.4Ga的古老碎屑锆石εHf(t)=-8.6~-4.6,揭示中、南部地区存在古太古代地壳物质。新太古代早期2.9~2.7Ga的锆石εHf(t)以正值为主(占比85%),它们的t C DM=3190~2774Ma,与其结晶年龄相同或接近,证明华北克拉通南部在新太古代早期以新生地壳生长为主。新太古代晚期2.55~2.45Ga峰期的锆石也以正的εHf(t)值为主(占比69%),而2.15~2.0Ga峰期锆石的εHf(t)值大多偏负(占比56%),说明华北克拉通南部地区从新太古代末期的新生地壳增生为主伴有陆壳再造转变为古元古代中期以古老陆壳物质再造为主,并有少量新生陆壳增生;古元古代晚期~1.92Ga年龄峰期的碎屑锆石εHf(t)=-11.9~+2.0,揭示至古元古代末期华北克拉通中南部进入到以古老陆壳物质再造为主的演化阶段。
