黔西南戈塘-海子地区金矿控矿因素分析与成矿模式探讨

在对区内构造性质及组合特征实地调查研究的基础上,系统总结区内“断裂型”、“界面型”、“土型”三类型金矿赋矿地质体空间产出特征及分布规律,进而提出NE向海马谷断层及配套的次级断裂为戈塘地区金矿成矿流体的主要通道,戈塘背斜为成矿前构造,对后期的成矿流体运移起到汇聚作用,中上二叠统(P_(2)m,P_(3)l)之间的岩溶不整合面为区内金矿体主要就位空间。结合稀土元素、硫同位素、包裹体研究成果以及区域航磁、重力特征,认为区内金矿为与深源岩浆活动有关、受NE向大型逆冲断层及其配套构造联合控制,具有“断裂+多层界面”矿体空间就位特征的中低温热液型金矿床。

黔西南海子地区土壤地球化学特征及金矿找矿方向探讨

本文通过对黔西南海子地区土壤地球化学特征的论述,结合区域成矿地质背景及金矿床地质特征进行综合分析,提出了区内的金矿找矿方向:北东向断裂带以及断层附近的有利岩性组合界面,主攻区域应首选HTZ-1、HTZ-2、HTZ-3综合异常分布区。

海子地区马鼻疽的疫情监测

为了摸清海子地区马鼻疽的流行情况,笔者于2016-2017年,采用马鼻疽菌素点眼变态反应法分别对该地区3个村的马鼻疽流行情况进行了调查。结果发现:197匹马的马鼻疽检测结果均为阴性,表明海子地区没有发生马鼻疽流行。

昭通荷花-海子地区煤层气资源条件及主控地质因素

昭通荷花-海子地区煤层气资源封盖保存条件较好,且无大型地质构造运动和断裂带造成煤层气的大量逸散。主要煤层含气量虽小,但煤层厚度较大,埋藏浅。煤储层为含水性均压地层,煤层为低阶高渗的褐煤层,生气能力和对气体的吸附能力较弱,且煤层基本未进行开采,储层围岩封盖良好,封闭性较好,地质构造相对简单,对煤层气的保存比较有利;煤层气初放速度较快,残余气量较少,可采量比重大。具有较好的煤层气勘探开发前景。

四川理塘海子山地区放射性地球物理特征

为研究四川理塘海子山地区放射性地球物理特征及铀成矿地质背景和成矿条件,在区内开展了地面伽马总量面积测量和地质-伽马能谱综合剖面测量。通过地面伽马总量面积测量,了解了海子山地区的伽马放射性背景,分析了其放射性特征;通过地质-伽马能谱综合剖面测量,初步判定了研究区内燕山晚期花岗岩的放射性异常性质,分析了各主要地层岩石的放射性核素含量特征。研究表明:区内出露的燕山晚期花岗岩有较高的伽马总量背景值,且伽马总量异常的展布与燕山晚期花岗岩体的分布特征基本一致;花岗岩体的铀含量背景值较高,显示了区内良好的铀源条件;研究区外围西侧有与NE向的断裂破碎带有关的查清卡温泉异常点,地表泉华具有极高的伽马总量测量值,且伽马能谱测量显示其为铀、钍混合异常点。根据查清卡温泉异常点的地质和放射性特征,并结合研究区铀成矿地质背景和成矿条件,初步判定本区铀源可能为深部含铀流体或铀富集在深部燕山晚期花岗岩体中,铀元素通过泉水迁移至地表沉淀富集,提供了下一步铀矿找矿方向。

Analysis to the Driving Force Model and Driving Factor on the Utilized Changes of Cultivated Land in Gonghe County

Using gradually regression analysis to establish the driving force model of utilized change of cultivated land in Gonghe County, and using path analysis, correlation analysis, partial correlation analysis and system dynamics method to inspect the effect of driving changing on cultivated land change under different change situations. Driving factors, action mechanism and process of utilized change of cultivated land were analyzed from the county territory scale level. At last, some corresponding policies and measures were put forward.

Groundwater Waves in a Coastal Fractured Aquifer of the Third Phase Qinshan Nuclear Power Engineering Field

Tidal fluctuations of Hangzhou Bay produce progressive pressure waves in adjacent field fractured aquifers, as the pressure waves propagate, groundwater levels and hydraulic gradients continuously fluctuate. The effect of tidal fluctuations on groundwater flow can be determined using the mean hydraulic gradient that can be calculated by comparing mean ground and surface water elevations.Tidal fluctuation is shown to affect the piezometer readings taken in a nearshore fractured aquifer around the nuclear power engineering field. Continuous monitoring of a network of seven piezometers provided relations between the tidal cycle and the piezometer readings. The relations can be expressed in times of a time and amplitude scaling factor. The time lag and the tidal efficiency factor and wavelength are calculated using these parameters. It provides significant scientific basis to prevent tide and groundwater for the nuclear power engineering construction and safety run of nuclear power station in the future.

Variations in leaf characteristics of three species of angiosperms with changing of altitude in Qilian Mountains and their inland high-altitude pattern

In this study, 39 leaf samples of three angiosperms （Betula albo-sinensis, tree species; and Caragana jubata and Berberis diaphana, shrub species） were collected in the middle-east parts at 2300-3640 m asl of the Qilian Mountains to study the varia- tions of leaf characteristics of angiosperms with altitude change in inland high-altitude regions of China. Five leaf indexes, viz. epidermal cell density （ED）, stomatal density （SD）, stomatal index （SI）, leaf vein density （VD） and carbon isotopic ratio （c^13C） were analyzed in laboratory. The results show that there are significant or even very significant linear correlations between the five indexes and altitude, of which SD, SI and VD exhibit a negative correlation with altitude, while ED and Ot3C exhibit a positive correlation with altitude. Such a correlation assemblage is quite different from the situation in the low-altitude humid environment. Generally, only an assemblage of positive correlations can be observed between the indexes （viz. SD, SI and （~3C, etc.） and the altitude in the low-altitude humid environment, which were caused mainly by the plants＇ responses to the change of atmospheric CO2 concentration （Co）. However, an assemblage of the negative and positive correlations found here may be attributed mainly to the plants＇ responses to the change of physiological drought caused by change of low temperature, and here it is preliminarily called the inland high-altitude pattern of plant leaf variations.

Some properties of field-aligned electron events in high-altitude polar regions

Using data from the Cluster spacecraft from January 2003 to December 2004, we perform a statistical study on some properties of the field-aligned electron(FAE) events and interplanetary magnetic field(IMF) By dependence of FAE events with different durations in high-altitude polar regions. A total of 1335 FAE events were observed by the C3 spacecraft. More down-flowing events were observed in the Southern Hemisphere, and more up-flowing events were observed in the Northern Hemisphere. It proves that down-flowing events mainly originate from magnetosphere or solar wind and up-flowing events are mainly derived from ionosphere. Short-lifetime events showed a morning concentration in the magnetic local time distribution, and long-lifetime events were concentrated both before and after noon. For the IMF By dependence of the FAE events, short-lifetime events were much affected by IMF By and resulted in a morning concentration, while the long-lifetime events were almost unaffected by IMF By. With further analysis, we determined that the short-lifetime and long-lifetime events had different sources.

Characteristics of low altitude ionospheric electric field over Hainan Island,China

A sounding rocket experiment undertaken by the Chinese Meridian Project from a low latitude station on Hainan Island(19.5°N,109.1°E),China,measured the DC electric field during 05:45-05:52 LT on April 5,2013.The data observed using a set of electric field double probes,as part of the rocket's scientific payload,revealed the special profile of how the vectors of the DC electric field vary with altitude between 130 and 190 km.During the experiment,the vertical electric field was downward,and the maximum vertical electric field was nearly 5.1 mV/m near the altitude of 176 km.The zonal electric field was eastward and slightly less than 0.6 mV/m.The plasma drift velocity was estimated from the E×B motion,and the zonal drift velocity was eastward and of the order of 100 m/s.The zonal wind velocity was also estimated using the drift velocity near the maximum density height in the F1-region,and it was found to be nearly 120 m/s.This work constituted the first in situ measurement of the DC electric field conducted within the Fl-region(between 130 and 190 km) in the East Asian Sector.

Chloride ion ingress distribution within an alternate wetting-drying marine environment area

Concrete structures in an alternate wetting-drying area often suffer from severe chloride ion ingress more than those in other areas. Field tests of marine structures were conducted, and chloride concentration is found to reach a maximum value at a certain elevation. The surface concentration and diffusion coefficient of chloride ions at different elevations exhibit Gaussian unimodal curve distributions. Using the chloride ion unsaturated permeability model, the distribution regularity mechanism is analyzed. Finally, an improved indoor accelerated simulation experiment is proposed to simulate the rules governing chloride ion ingress into concrete structures in an alternate wetting-drying area.

Effect of opening the Drake Passage on the oceanic general circulation:A box model study

The impacts of opening the Drake Passage(DP) on the oceanic general circulation are examined.When the DP is open,wind stress at mid-and high latitudes gives rise to a wind-driven gyre,which induces a meridional heat exchange between mid-and high latitudes in the Southern Ocean.After the opening of the DP,the Antarctic Circumpolar Current(ACC) forms and its associated strong temperature front blocks the heat transport from mid-latitudes to high latitudes.A simple box model is formulated,in which the effects of the wind stress(for the case of DP closed) and the thermal front(for the case of DP open) on the variability of Antarctic Bottom Water(AABW) and North Atlantic Deep Water(NADW) are explored.The sensitivity experiments demonstrate that:(1) When the DP is closed,the enhancement of the wind-driven gyre leads to the decline of AABW formation in the Southern Ocean and the increase of NADW formation in the North Atlantic.As a result,water in high latitudes of the Southern Ocean becomes warmer,so does the bottom water of global ocean.(2) When the DP is open,there is no formation of AABW until the intensity of thermal front along ACC exceeds a threshold value(it is 4.03℃ in our model).Before the formation of AABW,temperature in most of the oceans is higher than that after the formation of AABW,which usually leads to the cooling of high latitudes of the Southern Hemisphere and the bottom water in global ocean.When the strength of the thermal front is lower than the critical value,there is no AABW formation,and temperature in most of the oceans is slightly higher.These results demonstrate that during the opening of the DP,changes in wind stress and the formation of the thermal front in the Southern Ocean can substantially affect the formation of AABW and NADW,thus changing the state of meridional overturning circulation in the global ocean.