1) Shengyuan volcanic basin
盛源火山盆地
2) Shengyuan basin
盛源盆地
1.
Mineralogy evidence of shoshonite rock series from Shengyuan basin and it s adjacent area;
盛源盆地及邻区橄榄玄粗岩系列火山岩的矿物学证据及成因探讨
2.
Using the modern structural analysis on the characteristics of basement lithologics and lithofacies, basement structures and its evolution regularities the author suggests that the metamorphic deformed basement of Shengyuan basin creats extremely favourable geologic background for the ore formation of uranium and polymetal.
作者运用现代构造分析方法 ,侧重于基底岩性岩相特征、基底构造及演化规律的分析 ,认为盛源盆地变质变形基底为铀及多金属成矿创造了极有利的背景条件 ,据此建立起盆地的找矿模式 ,指出找矿方向。
3.
Based on the isotopic dating data of volcanics and recent research achievements of age boundary between Jurassic and Cretaceous systems, it is suggested that the volcanic series in Shengyuan basin must be attributed to Lower Cretaceous.
本文根据盛源盆地火山岩同位素年龄数据和侏罗 白垩系界线年龄的最新研究成果 ,认为盛源盆地火山岩系的地层时代应属早白垩世。
3) volcanic basin
火山盆地
1.
Strike-slip pull-apart process and emplacement of Xiangshan uranium-producing volcanic basin;
走滑拉分作用与相山产铀火山盆地的就位
2.
Geological conditions for ore-forming process and prospecting direction of the U-Mo polymetallic deposits in Guyuan volcanic basin;
沽源火山盆地铀钼多金属成矿地质条件分析及找矿方向
3.
Lingquan volcanic basin is located in the mid-southern segment of known Rrguna-Kelulun Eastnorth-trending volcanic rocks uranium metallogenic belt,it is on the same belt with Telechuf Field of Russia and Durnuot Field of Mongolia.
灵泉火山盆地位于著名的额尔古纳—克鲁伦北东向火山岩铀成矿带中南段,与俄罗斯斯特列措夫铀矿田、蒙古多尔诺特铀矿田处于同一矿带上。
4) volcanic basin
火山岩盆地
1.
New discovery and understanding about seeking the copper-lead-zinc polymetal deposits in volcanic basin of east Guangdong;
粤东火山岩盆地铜-铅-锌多金属矿床找矿新发现与认识
2.
Correspondingly, basins in the region evolved from the marine basin of Sinian to middle Triassic,the arround Yangtze foreland basin of late Triassic to middle Jurassic, volcanic basins of late Jurassic to early Cretaceous to extensional basins of late Cretaceous to Eogene.
下扬子地区震旦纪以来经历了不同的大地构造与地球动力学背景 ,盆地演化相应地经历了震旦纪—中三叠世海盆→晚三叠世—中侏罗世沿江前陆盆地→晚侏罗世—早白垩世火山岩盆地→晚白垩世—早第三纪陆相伸展盆地。
3.
Zouping copper deposit locates in Zouping volcanic basin in south part of Qihe-Guangrao deep fault belt.
邹平铜矿处于齐河-广饶深大断裂带南部的邹平火山岩盆地中,形成于破火山口火山通道充填的石英正长闪长岩岩颈中央上部,包括伟晶岩型铜矿和细脉浸染状斑铜矿床两种类型。
5) Fenghuoshan basin
风火山盆地
1.
Granulometric feature and depositional environment of Cretaceous period sandstone of Fenghuoshan basin in the Hoh Xil,Qinghai-Tibet plateau;
青藏高原可可西里风火山盆地白垩纪砂岩粒度特征与沉积环境
2.
Through the research on formation processes of basin, this article indicated that Fenghuoshan basin has passed four stages: basement, palaeogeomorphology basin, sedimentary basin and structural basin, formed in late Cretaceous deposit.
通过对盆地形成过程的研究,认为风火山盆地经历了基底、古地貌盆地、沉积盆地及构造盆地4个阶段,在晚白垩世沉积形成。
6) Egongshan volcanic basin
鹅公山火山盆地
补充资料：法盛《名僧传》
【法盛《名僧传》】
法盛。本姓李。垄西人。寓于高昌。九岁出家。勤精读诵。每曰。吾三坚未树。五众生灭。合会有离。皆由痴爱。若不断三毒。何求勉脱。年造十九。遇沙门智猛。从外国还。述诸神迹。因有志焉。辞二亲。率师友。与二十九人。远。诣天竺。经历诸国。寻觅遗灵。及诸应瑞。礼拜供养。以申三业。□忧长国东北。见牛头栴繵弥勒像。身高八寻。一寻是此国一丈也。佛灭度后四百八十年中。有罗汉名可利难陀。为济人故。舛兜率天。写佛真形。印此像也。常放光明。四众伎乐四时笑乐。远人皆卒从像悔过。愿无不克。得初道果。岁有十数。盛与诸方道俗五百人愿求舍身。必见弥勒。此愿可谐。香烟右旋。须臾众烟合成一盖。右转三币。渐渐消尽(云云)
法盛。本姓李。垄西人。寓于高昌。九岁出家。勤精读诵。每曰。吾三坚未树。五众生灭。合会有离。皆由痴爱。若不断三毒。何求勉脱。年造十九。遇沙门智猛。从外国还。述诸神迹。因有志焉。辞二亲。率师友。与二十九人。远。诣天竺。经历诸国。寻觅遗灵。及诸应瑞。礼拜供养。以申三业。□忧长国东北。见牛头栴繵弥勒像。身高八寻。一寻是此国一丈也。佛灭度后四百八十年中。有罗汉名可利难陀。为济人故。舛兜率天。写佛真形。印此像也。常放光明。四众伎乐四时笑乐。远人皆卒从像悔过。愿无不克。得初道果。岁有十数。盛与诸方道俗五百人愿求舍身。必见弥勒。此愿可谐。香烟右旋。须臾众烟合成一盖。右转三币。渐渐消尽(云云)
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参考词条