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1.
LIUGuo-ming ZHANGHeng-rong KONGQing-jun WUCheng-zhi GUOFeng ZHANGChao-fan 《东北亚地学研究》2004,7(2):156-160
Tianchi Volcano is the largest potential erupticve volcano in China. Analyzing these data on seismic monitoring, deformation observation and water chemistry investigation gained from the Tianchi Volcano Observatory (TVO), the authors consider that the Tianchi Volcano is in going into a new flourishing time. 相似文献
2.
WEIHai-quan JINBo-lu LIUYong-shun 《东北亚地学研究》2004,7(1):28-35
A number of different lahars have been recognized from a systematic survey of a mapping project. The high setting temporamre feature of the deposits indicates a relationship between the lahar and the Millennium eruption event of Tianchi Volcano. The lahars caused a dramatic disaster. Recognize of the huge avalanche scars and deposits around Tianchi Volcano imply another highly destructive hazard. Three types of different texture of the avalanche deposits have been recognized. There was often magma mixing processes during the Millennium eruption of Tianchi Volcano, indicating a mixing and co-eruption regime of the eruption. 相似文献
3.
A number of different lahars have been recognized from a systematic survey of a mapping project. The high setting temperature feature of the deposits indicates a relationship between the lahar and the Millennium eruption event of Tianchi Volcano. The lahars caused a dramatic disaster. Recognize of the huge avalanche scars and deposits around Tianchi Volcano imply another highly destructive hazard. Three types of different texture of the avalanche deposits have been recognized. There was often magma mixing processes during the Millennium eruption of Tianchi Volcano, indicating a mixing and co-eruption regime of the eruption. 相似文献
4.
LIU Guoming YANG Jingkui WANG Lijuan SUN Jicai .Changbaishan Tianchi Volcano Observatory Antu Jilin China .Seismological Bureau of Jilin Province Changchun 《东北亚地学研究》2011,(1)
Changbaishan volcano is the largest potential eruptive volcano in China.In this paper,seismic activity,horizontal displacement,vertical displacement and the fluid geochemistry data acquiring from Changbaishan Tianchi Volcano Observatory(TVO) in recent years are analyzed.The authors discussed the ability for the Changbaishan volcanic seismic monitoring and active level of Changbaishan volcano in recent years based on the fundamental monitoring results.The results show that Changbaishan volcano has experience... 相似文献
5.
Changbaishan volcano is the largest potential eruptive volcano in China.In this paper,seismic activity,horizontal displacement,vertical displacement and the fluid geochemistry data acquiring from Changbaishan Tianchi Volcano Observatory(TVO) in recent years are analyzed.The authors discussed the ability for the Changbaishan volcanic seismic monitoring and active level of Changbaishan volcano in recent years based on the fundamental monitoring results.The results show that Changbaishan volcano has experienced an unrest episode from 2002 to 2005,but its active level recovers to the background now. 相似文献
6.
The huge comendite ignimbrite- forming eruption of Tianchi Volcano maintained a stable plinian column during its earlier stage of eruption, and succeeded a collapsing of the column producing pumiceous ignimbrite deposits. It is estimated that the column height (Hb) varied from 20km to 10km in its eruption period, with a maximum height of 25km in the eruption peak. Its umbrella cloud spread into the stratosphere with a top height of 35km (Ht). The dense lithics whose diameter exceeded 8cm followed a ballistics trajectory in a 3km - high gas thrust region, while the smaller lithics and pumices entered the convection region in the column. The initial magma temperature was 780℃. The comendite magma had an exit velocity of 300m/s, volatile content of about 1wt% and lithics of 8.5wt%. From a 400m - wide vent the magma was expelled out with a mass eruption rate of 108.36kg/s, corresponding to a volume rate of 104.95m3/s. Over 1. 3436 × 1019J of energy had been released from Tianchi Volcano, of which the kinetic proportion was about 8 %. The plume had a temperature of -50℃ at the base focus of the cloud and a upward speed of 215m/s. The cloud spread out at a gradually downspeed with the increasement of distance from its center. For example, at a distance of 25km from its center the spreading velocity is about 250m/s, and is about 60m/s at distance of 100km. The main part of the plinian column, that is the convection region, once occurred in the height between 3 to 25km, and its maximum width was about 13km in radius. 相似文献
7.
11 samples of lava and pumice from the cone of Changbaishan Tianchi Volcano, Jiling, China, were dated by using high precision U - series TIMS method. We conclude that the bottom of the cone formed before 350 ka, the middle part in 70～80 ka, the upper during 20～ 1ka, and the top less than 1ka, and the age based periods of the volcano eruption since Late Pleistocene is given as follows: ＞ 350ka, 70ka, 18 ～ 25ka, 10ka, 4C5ka, 1～0.75ka, which may offer the basis for the study of volcanic disaster in future. In addition, the principle of dating young volcanic rocks by using U - series TIMS method is introduced briefly. Differentiation characteristics of U and Th in different minerals of the volcanic rocks are discussed, and the ability producing isochrons, based on U and Th differentiation, are discussed. In the last part of the paper,the closure of samples to the elements U and Th, which is important for age results, is discussed by using (234U/238U)radioactivity ratio which can be used to monitor if the samples have been weathered or eroded or leached since the time they formed. In this study, all samples have (234U/238U) activity ratios within 1% of secular equilibrium ((234U/238U) radioactivity ratios are unity), indicating no disturbance of the 234U- 238U system. All of these discussions show that the TIMS method is good to date Tianchi volcanics and the results are reliable. 相似文献
8.
长白山火山区几何形变的联合反演 总被引：13，自引：1，他引：12
应用长白山火山区的水准和GPS资料，采用Mogi源模型对火山区的压力源参数进行联合反演，并考虑天池火山南侧断层的影响，利用Okada的断层位错模型对长白山火山区近年来的主要活动区天池火山的地下岩浆的可能变化进行推测，得出以下结论：长白山天池火山浅层目前为单一的压力源，位置仍在天池老火山口一带；近几年岩浆上涌活动比较明显；天池南侧的北西向隐伏断裂有一定的活动性。 相似文献
9.
Neil B. McLaughlin 《山地科学学报》2011,(5)
Geohazards appear to be increasing in frequency globally. It is of necessity to actively manage these natural hazards to minimize loss of life and property. From an early warning perspective, this paper stresses the potential fatal flood hazard represented by the huge volume of water in Tianchi Lake, the unique geography of Changbai Mountain, and the limited flood control ability in the upstream of the Songhua River. Northeast Asian countries should keep a watchful eye on the Changbai volcano cooperatively,... 相似文献
10.
11.
Mohammed Hazaea HU Ke Mohammed Mattash CHEN Bing M.O.Al-Jabali Aref Mohammed Abdussalam 《世界地质(英文版)》2004,7(2)
The chemical composition of several thermal springs around Changbaishan area has been investigated.Cenozoic basaltic rocks are widely distributed in Northeast China and geothermal characteristics have been described.About one hundred hot springs exist around Changbaishan Volcano at the border between China and D.P.R.Korea with high temperature about 82℃. The pH values of the spring water range from 6.9 to 7.1 and the total flow rate is about 4.8 L /sec. The chemical composition of the thermal springs is sodium carbonate; the high-mineral contents of thermal water are believed to have medicinal properties. Bathhouses are already built along the hot springs to take the advantage of the supposed healing properties. The high quality of those hot springs is believed to be utilitized for mineral water. The chemical equilibrium temperatures were estimated at about 160℃ based on the Na-K-Ca geochemical thermometer. 相似文献
12.
用1961—2008年NOAA的月平均再分析资料和1980—2006年云南5个探空站的资料,采用大气可降水量和水汽通量公式计算分析大气可降水量和水汽通量,并用线性趋势分析其变化特征。结果表明：云南四季的可降水量北少南多,呈“u”型分布,夏季最大,冬季最小。对云南地区四季的水汽通量分析表明,四季的水汽净收入主要集中在对流层低层;地面-300hPa的水汽净收入在夏季最大、秋季次之,而冬季最小。云南经向的水汽输送和纬向的水汽输送呈反相关,近48年,云南四季水汽呈增加趋势,其中夏季增加最多,春季次之。 相似文献
13.
鄂尔多斯盆地南部旬邑-宜君地区中生界储层特征 总被引：1，自引：0，他引：1
对鄂尔多斯盆地南部旬邑 -宜君地区中生界主要储集层——直罗组、延安组、延长组储层特征从沉积相、砂体纵向展布、岩性和物性等几方面进行了简要论述。通过研究指出本区储层具有低孔、低渗的特点。在纵向上以直罗组储层相对最好 ,延安组次之 ,之后才是三叠系延长组。储集层普遍具有岩性细、成岩后生变化强烈的特点。由于储层低孔、低渗 ,因此 ,油层的压裂改造措施必不可少 相似文献
14.
采用商河县2010年耕地地力评价有机质采样点的数据,运用GIS和地统计学相结合的方法,研究了商河县土壤有机质的密度及储量,并按照土类统计分析了不同土壤类型间的有机碳密度及储量差异。研究表明,商河县土壤有机碳密度范围为1.69~5.17kg/m2,平均3.44kg/m2;有机碳储量为0.26×1010kg。按乡镇统计,有机碳密度最大值为玉皇庙镇3.65kg/m2,最小值为郑陆镇3.15kg/m2,有机碳储量最大值玉皇庙镇3.47×108 kg,最小值张坊乡0.92×108 kg;按土壤类型统计,有机碳密度最大的为湿潮土3.46kg/m2,最小为风沙土3.29kg/m2,有机碳储量最大为潮土10.38×108 kg,最小为褐土化潮土1.34×108 kg。 相似文献
15.
为了查明昌乐县五图煤田古近纪李家崖组油页岩的分布及其品质特征,从沉积学、油气地质学等方面开展研究。五图煤田古近纪李家崖组可划分为4部分:上部含煤段(A),中部含煤段(B)、油页岩段(C)和下部含煤段(D)。该组油页岩主要发育在淡水湖相沼泽环境,油页岩发育层数较多,可达80余层,但单层厚度不大。基于对大量钻孔的油页岩厚度统计及相关的化验测试,研究发现:李家崖组油页岩总厚度在研究区中部靠近南侧F3断裂处厚度最大,向四周减薄;灰分平均含量60%左右,靠近北侧F1断裂处灰分较高;焦油产率平均约8.36%,靠近南部F3断裂附近产率较高;硫分平均含量2.14%,水分平均含量4.2%,硫分和水分含量整体表现为东南部高西北部低。综合研究可以发现,研究区中南部靠近F3的地区,油页岩厚度大、品质好,是五图煤田油页岩资源潜力区。 相似文献
16.
五图煤矿油页岩广泛分布于李家崖组的B段、C段和D段,以C段为主体,探明储量2.72亿t,是褐煤的伴生矿种。C段油页岩层密集,厚度大;D段上部含油页岩,但厚度小。油页岩焦油产率最高16.25%,最低5.43%,平均8.36%。基准发热量最高8.72MJ/kg,最低6.16MJ/kg,平均6.91MJ/kg。油页岩作为固态燃料,是汽油的替代能源,五图煤田油页岩资源的开发和利用前景广阔。 相似文献
17.
???ú??CORS?????????4???GPS????????????GAMIT/GLOBK??????е??????????????????????????????????????????????????????????????????????????3???????????????150 mm??11?′??????????4??????????????????10 mm/a????????溯?????????????????????????????????6′×6′????????????????????????????????? 相似文献
18.
使用GAMIT/GLOBK解算2006~2015年覆盖四川地区的50个CORS站的观测数据,并提取坐标时间序列,获得速度场模型。对四川省整体地壳运动以及区域应变场进行分析,结果表明,四川省CORS站水平方向平均速度为38.72 mm/a,速度场的优势方向为S73.9°E;欧亚框架下水平方向平均速度为14.40 mm/a,优势方向为S77.78°E,较ITRF2008框架下的速度降低了24.32 mm/a;垂直方向平均速度为3.43 mm/a,整体上表现为隆升状态,位于东部平原的少部分测站处于下降趋势,可能是由于城市建设、地下水或者煤矿、石油等自然资源的过度采伐导致;最大主应变率达到7.31×10-11/a,最小主应变率为-5.4×10-11/a,其中区域地壳面膨胀率高值区域集中在川西,低值区域和最大剪切应变率高值区域分布在三大断裂带附近。 相似文献
19.
宁阳县东谷堆铁矿化属晚期岩浆液态分异的熔离矿化,铁矿化体赋存于麻塔单元粗粒变角闪石岩内,矿床由3个矿化体组成,各矿化体相间分布,总体走向均为NW向。矿石自然类型有磁铁阳起角闪石岩、磁铁黑云角闪石岩。矿石矿物以磁铁矿为主,脉石矿物主要为角闪石。矿石具柱粒状变晶结构、鳞片变晶结构、包含结构,浸染状构造、块状构造。矿石品位低,全铁含量一般13.5%~16.5%,最高达19.76%。矿床平均品位TFe15.15%,SFe8.26%。矿化体裸露地表,适宜露天开采。矿石加工技术性能良好,采用二次精选,一次扫选半闭路式选矿工艺流程。选石结果为:精矿全铁含量62.10%,精矿率11%~12%,回收率31.40%。 相似文献
20.
黄岗潜凹陷岩盐矿床是山东省地质科学研究院近年发现的一大型岩盐矿产地,预测岩盐矿总资源量超过240×10~8t。本文在总结黄岗潜凹陷岩盐矿勘查成果的基础上,对区内岩盐矿沉积地质特征及成矿规律、岩相分布规律等进行了初步总结分析。岩盐矿赋矿层位为古近纪官庄群大汶口组中段,岩性为深灰色泥岩、粉砂质泥岩与灰白色膏质泥岩、石盐岩互层,是一套含石盐、石膏的浅湖—咸湖相沉积建造,其盖层为新近纪黄骅群和第四系。岩盐矿层赋存形态简单,呈层状产出,产状稳定,走向近EW向,倾向近S向,倾角平缓,一般3°,局部断层附近可达10°。区内揭露岩盐矿层31层,埋深1079.75～1730.86m,单矿层平均厚度0.25～24.64m,单层最厚53.96m,累计平均厚度175.45m,单孔累计最大厚度320.23m,是山东迄今单孔控制最大的厚度,NaCl平均品位44.11%～96.08%。岩盐矿石矿物成分较为简单,主要盐类矿物成分为石盐和硬石膏,杂质矿物主要为黏土质矿物;矿石主要化学组分为NaCl,其次为CaSO_4,其他组分含量甚微;矿石结构主要为中粗粒他形—半自形粒状结构,矿石构造主要为块状构造;岩盐矿划分为结晶块状石盐矿石和石膏石盐混生石盐矿石2种自然类型,矿石工业类型初步确定为石膏质石盐矿石。黄岗潜凹陷盆地为一套浅湖—咸湖相沉积,大致反映了含盐水体淡化—浓缩—淡化的蒸发沉积过程;平面上初步划分石盐岩相区和膏泥岩相区2个岩相分布区,其中石盐岩相区靠近成盐盆地局部沉积中心,发育厚层岩盐矿。黄岗潜凹陷西南部含盐地层总体表现为向南倾伏的单斜形态;区域重力资料显示,该区靠近盆地局部沉积中心,具有较大的岩盐矿找矿潜力。区内岩盐矿层厚、质纯、埋深适中,初步评价具备建设盐穴储气储能库的地质条件,矿床开发利用前景广阔。 相似文献