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11.
Zhou Zhaode 《地理学报(英文版)》1994,(Z1)
I.Introducti0I1Hail1al1isthelargnsttropicalislal1dwitllabundal1t11aturalrcsourccssuitablef0rgrowtllgtrol,icalcropsand\\4t11ven'highp0tentia1pr0d,uctivity.Hotx'cY'cr,t11c1-ca1'cstillsomeproblemsf(l)Tl1ese1ectionoflandsuitableforfqrestisn0tstrictalldPreservativerateoftr0picalcr0psislow,(2)Mostoftropicalcr0psarecollccntratcdillthezoneofeastern"windgap"andnorthern"frigidplace"andtheirsecurityisnotstable,(3)Rubberareaaccountsforab0uttwo-thirdsoftl1etotalarea0ftropica1crops,henceproportiondis1ocat… 相似文献
12.
本文从海南热带作物生物特性、现实生产结构和地区气候条件出发、对热作种植业进行了模湖区域性划分；在计算构成各区产量基本参数的基础上，应用多目标规划方法，建立了热作结构优化的近期分区模型；并通过近期基础模型和对未来参数的预测，建立了远期灰色规划模型。结果表明，近期方案可提高收益5．1－55．7％，远期方案可提高54－90％，远近期方案均取得了明显的经济效果。 相似文献
13.
新疆北山地区红石山岩体橄榄石与铬尖晶石成分特征及成因意义 总被引：1，自引：0，他引：1
红石山镁铁质-超镁铁质岩体,位于塔里木板块东北部的新疆北山地区,岩体平面为长条状,出露面积大于100 km2。岩体的堆晶韵律和堆晶旋回发育,属典型的层状岩体,每个旋回之间为突变接触关系,旋回内部为迅速或渐变过渡关系。岩石类型丰富,主要有纯橄岩、(含长)单辉橄榄岩、橄长岩、橄榄辉长岩、辉长岩和少量辉石岩。橄榄石和铬尖晶石是重要的早期结晶矿物。通过电子探针分析证明:橄榄石的Fo值为76~90.2,总体上随基性程度的降低,Fo降低。铬尖晶石Cr#为54~69,变化范围较小,落于典型层状岩体的铬尖晶石组成范围。模拟计算表明,形成红石山岩体的地幔部分熔融程度高(17.29%~18.92%,平均为18.41%)、原生岩浆为高温(1 290℃~1 330℃)、高镁(Mg O=13.63%)的苦橄质岩浆,这为塔里木二叠纪地幔柱活动提供了新的证据。 相似文献
14.
塔合曼滑坡体是发育在新疆帕米尔高原东部1895年塔什库尔干7级地震区北端的一个大型滑坡体,总体呈“舌”形,由崩塌区、滑坡区和堆积区三部分组成,在滑坡区和堆积区分别形成了平行与垂直于滑坡体滑动方向的滑坡体台阶.本文介绍了该滑坡体的基本特征并采用宇宙成因核素测年技术对其形成年代进行了测定,简要论述了该测年技术的基本原理、野外采样原则及样品前处理过程.采自滑坡体不同部位的6个片麻岩巨砾样品的10Be暴露年龄结果非常一致,表明该滑坡体发生在6.8±0.2ka,同时也表明了10Be暴露测年是研究大型滑坡的有效测年手段.结合该滑坡体被慕士塔格断层断错并形成断层陡坎、滑坡体内发育的冲沟规模以及巨砾表面较厚的岩石漆,我们认为该滑坡体并非1895年地震的产物. 相似文献
15.
DU Wei JIANG Changyi Tang Zhongli XIA Mingzhe XIA Zhaode LING Jinlan ZHOU Wei WANG Bangyao 《《地质学报》英文版》2017,91(3):1153-1154
<正>Objective Eclogites are important indicators of ancient plate boundaries or paleosuture zones.Despite their great geological significance,very few investigations have been carried out in the Kunlun region.The Central East Kunlun fault zone was believed to be an Early Paleozoic suture zone,but there has been no reliable evidence for this,though studies on ophiolite,granite,and basic granulite indicate that the Early Paleozoic orogeny occurred in the East Kunlun.This work focused on the Dagele eclogites in 相似文献
16.
山东省城市经济效率分析 总被引：7，自引：1，他引：6
应用城市整体效率指标,对山东省城市效率的规律进行定量分析,总结了全省城市效率呈现规模效果梯度的结构特点和地域分异规律,并对山东省未来城市化提出建议。 相似文献
17.
Yuan Zhaode Liu-Zeng Jing Zhou You Li Zhigang Wang Heng Yao Wenqian Han Longfei 《中国科学:地球科学(英文版)》2020,63(1):93-107
The Altyn Tagh fault is one of the few great active strike-slip faults in the world. The recurrence characteristics of paleoearthquakes on this fault are still poorly understood due to the lack of paleoseismic records recorded in high-resolution strata. We document a paleoseismic record in a pull-apart basin along the Wuzunxiaoer section of the central Altyn Tagh fault.The high-resolution strata recorded abundant seismic deformations and their sedimentary responses. Four earthquakes are identified based on event evidence in the form of open fissures, thickened strata, angular unconformities, and folds. The occurrence times of the four events were constrained using radiocarbon dating. Event W1 occurred at AD1220–1773, events W2 and W3 occurred between 407 and 215 BC, and event W4 occurred slightly earlier at 1608–1462 BC, indicating clustered recurrence characteristics. A comparison of the earthquake records along the Wuzunxiaoer section with other records along the Xorkoli section suggests that both sections ruptured during the most recent event. 相似文献
18.
为评估滆湖围网拆除工程实施效果,采用高密度网格化布点方法,系统分析滆湖沉积物营养盐和重金属的空间分布和污染特征;并基于有机氮评价方法、综合污染指数评价方法、重金属地质累积指数法和重金属潜在生态风险评价方法进行污染风险评价.结果表明,滆湖沉积物总氮(TN)、总磷(TP)和总有机碳(TOC)的平均含量分别为(3709±1004)mg/kg、(1127±650) mg/kg和(78.39±23.88) mg/g,三者空间分布特征较为一致;营养盐综合污染指数评价表明,全湖整体为重度污染,其中全湖TN均处于重度污染状态,TP绝大部分区域也处于重度污染状态.沉积物重金属Zn、Cr、As、Pb、Ni、Cu、Cd 的平均含量分别为(170.62±47.25)、(105.18±34.91)、(68.55±10.86)、(52.43±14.73)、(44.04±11.93)、(42.57±12.43)、(1.55±1.06) mg/kg,整体上呈现出由南向北、自西向东逐渐增加的趋势,重金属含量最高值在湖区东北角;地积累指数法和潜在生态风险指数法评价结果均表明Cd和As是主要的生态风险贡献因子,其中Cr和Ni的污染程度表现为清洁,Cr、Ni、Cu、Zn和Pb的单项潜在生态风险等级表现为轻微风险.与围网拆除前比,湖中区西南部沉积物营养盐含量无显著变化,湖南区南部沉积物营养盐状况明显改善,但其余各区域沉积物营养盐状况均有不同程度的恶化;湖区沉积物中重金属元素平均含量均有极大程度的降低,降幅在29.50%～80.45%之间,表明在外源污染输入得到一定控制时,围网拆除在控氮、控磷效果及改善重金属污染状况方面有着积极作用. 相似文献
19.
SHEN Qiushi ZHANG Lu Ismael Aaron KIMIREI WANG Zhaode GAO Qun CHEN Shuang YU Cheng 《海洋湖沼学报（英文）》2019,(1):134-145
The vertical distributions of trace metals and physicochemical parameters in water columns in Kigoma Bay and Kungwe Bay in eastern Lake Tanganyika, Tanzania, were studied. The Al, Ba, Ca, Co,K, Mg, Mn, Mo, Na, Sn, Sr, and V concentrations were low and varied very little with depth. The toxic heavy metal(As, Cr, Cu, Ni, Pb, and Zn) concentrations were relatively high in the surface water, and the Cu, Ni, Pb, and Zn concentrations decreased with depth. Principal component and cluster analyses indicated that the metals in the lake had three main sources. Al, Ba, Ca, Co, Cu, Cr, Mn, Sr, Sn, and V were found to be geogenic; As, Cr, Cu, Mo, Ni, Pb, Sn and Zn anthropogenic; and As, Ca, Co, Mg, and Na biogenic.Human health risk assessments were performed, and it was found that trace metals in the water at most of the sampling sites would cause no potential adverse ef fects or non-carcinogenic health risks through dermal contact or ingestion. However, trace metals in surface water in Kungwe Bay could have certain adverse ef fects on human health through the ingestion pathway(the total hazard quotient for ingestion(ΣHQi ng)was 1.75(a value >1 was de?ned as possibly indicating adverse ef fects). The Pb HQi ng for surface water in Kungwe Bay was 1.50 and contributed >80% of the ΣHQ_(ing_, implying that Pb pollution is a water quality and safety problem that needs to be carefully monitored and the potential sources identi?ed. 相似文献
20.
Zhaode YUAN Jing LIU-ZENG Xue LI Jing XU Wenqian YAO Longfei HAN Tao LI 《中国科学:地球科学(英文版)》2021,64(1):127-147
Large-scale detailed mapping plays a key role in revealing the rupture characteristics and mechanisms of strong earthquakes.Relatively few studies have been performed on the surface ruptures of large earthquakes in central and western Tibet due to its remote nature and high elevation.Based on high-resolution unmanned aerial vehicle(UAV)photography,we mapped the coseismic surface rupture of the 2014 Yutian M_s7.3 earthquake.Along the western Altyn Tagh fault system,the earthquake produced~37 km of surface rupture along the South Xor Kol fault(southern section S1),Xor Kol fault(central section S2)and Ashikule fault(northern section S3).Section S1 has a 16-km-long surface rupture with an average sinistral offset of 52±25 cm and a maximum offset of~90 cm,while section S3 has a 14.2-km-long surface rupture with an average sinistral offset of 36±21 cm and a maximum offset of~84 cm.A compilation of 5308 cracks yields an average crack width along the southern section of 85±71 cm and a maximum width of~700 cm;the average width along the central section is 39±21 cm,and the maximum width is 243 cm;and the average width along the northern section is 61±44 cm with a maximum of~340 cm.In addition,the average cumulative opening across rupture zone is 3.4±2.9 m along the southern section,with a maximum of~17 m;4.3±3.6 m along the central section,with a maximum of~13 m;and 1.7±1.6 m along the northern section,with a maximum of~6 m.Evidently,the average crack width and cumulative opening decrease towards bends and steps along the fault.A global synthesis of surface rupture distributions corresponding to strike-slip earthquakes indicates that the rupture zone is wider near the complex parts of fault geometries(such as bends,steps and fault bifurcations)than along straight sections,suggesting that the fault geometry has an obvious control on the surface rupture width.The widespread cracks at the intersection between the Xor Kol and South Xor Kol faults may indicate that an extensional regime is more likely to produce distributed offfault deformation,which provides an observational constraint for the numerical simulation of dynamic rupture on a fault.In addition to coseismic surface rupture,the Yutian earthquake also produced a large number of gravity-driven slides on alluvial fans with gentle slopes.The friction efficiency of the water-bearing salt layer beneath fans could decrease the sliding threshold and trigger instability under surface shaking.These distributed deformations and gravity-driven slides reflect the coupling between the rupture propagation and fault geometry and indicate that the rupture may have propagated in two directions along the Ashikule fault after passing through a step.Therefore,the investigation of coseismic surface rupture provides important observational constraints on the dynamic rupture process. 相似文献