Crust-Mantle Structures and Gold Enrichment Mechanism of Mantle Fluid System

Gold enrichment mechanism of ore-forming fluid is the essence of gold metallization.This paper summarizes the distinguishing symbols of mantle fluid and effect of crust-mantle structure on fluid movement. Fluid moving processes include osmosis, surge, gas-liquid alterna-tion and mutation of fluid speed. During fluid movement, gold will be enriched gradually. Final-ly, a layered circulatory system is illustrated in this paper.     

Crust-Mantle Structure and Coupling Effects on Mineralization： An Example from J iaodong Gold Ore Deposits Concentrating Area, China

Based on the results of two-dimension velocity structure, 1 : 100 000 aeromagnetic anoma-ly, 1 : 200 000 bouguer gravity anomaly and seismic anisotropy of Jiaodong and neighboring region in Shandong, China, the information of geophysical field was divided into two parts: deep- and shallow-focus fields. And then, the information of two different fields was combined with that of deep-seated ge-ology and ore deposit features. The synthetic result was adopted to analyze three-dimension structure, to probe into crust-mantle coupling effects of mineralization and dynamics of ore formation system.     

Cenozoic Volcanism in South China Sea and Its Vicinity and South China Sea Spreading

The rock series, rock types and Sr-Nd isotopic dating of the Cenozoic volcanic rocks in the South China Sea are similar to those in its vicinity. On the basis of the spreading age of the South China Sea, the Cenozoic volcanic rocks are divided into three stages: the pre-spreading stage, the spreading stage and the post-spreading stage. The deep process characteristics of the asthenosphere and lithosphere may be inferred from the study on primary basaltic magma. The top layers of the asthenosphere both in the spreading stage and in the pre-spreading stage are closer to the earth surface than that in the post-spreading stage. From the pre-spreading stage to the spreading stage, the top layer of the asthenosphere decreased in depth, while the amount of interstitial partial melts increased. The evolution of the primary basaltic magma shows a progressive evolution sequence of the rifting volcanism and a faster lithospheric spreading velocity. From the spreading stage to the post-spreading stage, the top layer of the asthenosphere gradually increased in depth, but the amount of interstitial partial melts decreased. The evolution of primary basaltic magma shows a retrogressive evolution sequence of the rifting volcanism and a gradual decrease in the lithospheric spreading velocity. The depth recognized by the study on the Cenozoic volcanism demonstrates the deep environment for the formation and evolution of the South China Sea.     

Demarcating the worldwide monsoon

Summary The monsoon is a global climate phenomenon. This paper addresses the seasonal reversal of atmospheric circulation and the transition of dry/wet spells in the monsoon regions worldwide. The NCEP/NCAR 850 hPa wind reanalysis data for 1950–1999 and the upper-tropospheric water vapour (UTWV) band brightness temperature (BT) data observed by NOAA polar orbiting satellites for 1980–1995 are used. In the tropics, there are three large wet-UTWV centres. The summer monsoon in the subtropics can be defined as the expansion of these centres associated with the influence of cross-equatorial flows. Specifically, the dry/wet spell transition is determined by the BT values that are smaller than 244 K. The regions of the South and North African monsoons, the Asian-northwest Pacific and Australian-Southwest Pacific monsoons, and the North and South American monsoons are examined with a focus on the dry/wet spell transition and stream field features. Findings suggest that the summer monsoons over many subtropical regions can be defined by both cross-equatorial flows and dry/wet spell transitions. In the mid- and low-latitudes, there exist six major dry/wet spell transition regions with a dry or wet period lasting more than one month. The region of most significant change is located over the subtropical North Africa–Asia–northwest Pacific. The others appear over subtropical South Africa, Indonesia–Australia, southwest Pacific, the Mexico-Caribbean Sea, and subtropical South America. In addition, three regions exist where only one of the two indicators (cross-equatorial flow and dry/wet transition) is satisfied. The first is near the Equator where the directions of cross-equatorial flows alternate but a dry/wet spell transition is never experienced. The second is over North Africa where only the dry/wet spell transition can be found but not the cross-equatorial flows. The third is over the mid-latitude regions in North China, South Africa, and northern North America. These regions are influenced by cross-equatorial flows but the upper-tropospheric water vapour content is not as high as that in tropical regions. Received June 29, 2000 Revised May 15, 2001     

新时期市(地)县地震工作的展望

论述了新时期市（地）县地震工作的重要性和主要任务；提出了做好市（地）县地震工作的建议和措施。     

城市共享汽车分布的时空演变及影响因素研究——以北京市主城区为例

城市交通可持续发展的本质在于空间资源合理配置,共享汽车作为一种新型交通方式,探究其时空分布规律及影响因素,能支撑交通资源空间配置并优化城市功能布局。以供需理论为基础,运用核密度分析、空间自相关、标准差椭圆等方法反映时空特征,通过地理探测器从供给和需求2个维度,分别选取停车场、人口密度以及居住空间、就业空间、公共服务与活动空间等5方面,共14个代理变量探究时空格局形成的影响因素。结果表明：① 共享汽车分布具有显著的时空异质性,根据时空特征可分为“早晚”型、“日间”型、和“均匀”型3类集聚中心;② 出行需求是影响共享汽车空间分布的主要因素,其中购物场所、科教文化场所、医疗保健场所等公共服务和活动空间是共享汽车的主要目的地;③ 政府应进一步做到精准投放,将资源重点布局于“日间”型集聚中心、居住空间和公共服务与活动空间等,以此促进共享汽车可持续发展和城市空间布局优化。     

Flood assessment and early warning of the reoccurrence of river blockage at the Baige landslide

On 10th Oct.and 3rd Nov.2018,two successive landslides occurred in the Jinsha River catchment at Baige Village,Tibet Autonomous Region,China.The landslides blocked the major river and formed the barrier lake,which finally caused the huge flood disaster loss.The hillslope at Baige landslide site has been still deforming after the 2018 slidings,which is likely to fail and block the Jinsha River again in the future.Therefore the investigation of 2018 flood disaster at the Baige landslide is of a great significance to provide a classic case for flood assessment and early warning for the future disaster.The detailed survey revealed that the outstanding inundations induced bank collapse disasters upstream the Baige landslide dams,and the field investigations and hydrological simulation suggested that the downstream of the Baige landslide were seriously flooded due to the two periods of the outburst floods.On these bases,the early warning process of potential outburst floods at the Baige landslide was advised,which contains four stages:Outburst Flood Simulating Stage,Outburst Flood Fore-casting Stage,Emergency Plan and Emergency Evacuation Stage.The study offers a con-ceptual model for the mitigation of landslides and flood disasters in the high-relief mountain-ous region in Tibet.     

Identification and alleviation pathways of multidimensional poverty and relative poverty in counties of China

To realize efficient and sustainable poverty alleviation,this study firstly investigated the identification of multidimensional poverty and relative poverty,and then explored relevant poverty alleviation pathways.Poverty levels in 31 provinces including the autonomous re-gions and municipalities of China were identified at the county level using the average nighttime light index (ANLI),county multidimensional development index (CMDI),and a method combining multidimensional poverty index and relative poverty standards.Poverty alleviation pathways for poverty-stricken counties were explored from the aspects of industry,education,tourism and agriculture.The results revealed that nearly 60％ of counties in China were primarily under relative poverty,most of which were corresponded to light relative pov-erty.In terms of ANLI and CMDI,63％ and 79％ of the national poverty-stricken counties,as of 2018,could be identified,suggesting that CMDI had a higher performance for identifying poverty at the county level.In terms of poverty alleviation pathways,414,172,442,and 298 poverty-stricken counties were receptive to industry poverty alleviation,education poverty alleviation,tourism poverty alleviation,and agriculture poverty alleviation,and 61％ of coun-ties had more poverty-causing factors,implying that multidimensional poverty alleviation is suitable in most of the counties.     

Gradient Boosting Decision Tree for Lithology Identification with Well Logs: A Case Study of Zhaoxian Gold Deposit,Shandong Peninsula,China

Natural Resources Research - Identifying lithology from well logs is an important step in deep prospecting and resource estimation. Various machine learning algorithms have been adopted to identify...     

围栏引起的有蹄类动物死亡及其对未来祁连山国家公园管理的启示

围栏是牧区畜牧业的重要组成部分。但是,这些围栏也给野生动物带来了很多负面影响,会制约它们的活动范围,妨碍其种群扩散甚至会直接导致死亡。甘肃盐池湾国家级自然保护区未来将成为祁连山国家公园的重要组成部分,本文对该区内围栏的现状及其所产生的影响进行了评估。我们通过70份调查问卷,了解了当地牧民对围栏的看法、围栏对野生有蹄类动物的威胁以及观察到的被围栏缠绕的野生动物的数量。我们发现,如果当地居民发现用于管理牲畜的围栏会伤害到野生动物,他们更可能意识到围栏带来的负面影响,那些认为围栏对野生动物有害的人更有可能支持拆除围栏。然而,对于需要雇用他人来照看家畜的牧民,支持围栏拆除的可能性较小。最佳模型只解释了部分数据差异,这表明虽然对围栏威胁的认识很重要,但其他因素可能也会影响牧民对围栏拆除的支持度。因此,为了能在新的国家公园内成功开展围栏拆除工作,有必要强化社区服务和社区合作,以减少围栏拆除对牲畜管理的影响。调查发现,当地牧民在围栏上发现过死亡的藏野驴、盘羊和藏原羚,其中发现藏野驴的次数明显多于其他两个物种。这一结果表明,前述三个物种可能更容易被围栏缠绕,未来需要加强相关研究,这将有助于推动围栏拆除计划的实施。