求短文汉语翻译(英译汉)请各位高人出手相助! 50
MINERALIZATIONMineralizationconsistsofquartzveins,stockworks,veinlets,andfracturesbea...
MINERALIZATION
Mineralization consists of quartz veins, stockworks, veinlets, and fractures bearingmolybdenite, pyrite, magnetite, minor chalcopyrite, and rare bornite, bismuthite, galena,wulfenite, scheelite, and specularite. Quartz veins mineralized bymolybdenite occurmilky white to banded or ribboned and are often brecciated and healed by quartz and latestage calcite and minor chalcedony. Molybdenite varies in grain size from very coarse
and greasy to microscopic grains in quartz, referred toas "black quartz ore".Disseminated molybdenite mineralization occurs as broad halos around and between the veins in the Endako pit but is lacking in the Denak pits where discrete mineralized veins and narrow low grade envelopes are separated by waste (Figure 7-3). Individual quartzmolybdenite veins have limited extent; however, the vein systems in which they occur can be traced throughout the deposit (Bysouth and Wong, 1995).The pyrite zone lies to the south of and adjacent to the orebody and has a transitional boundary in the immediate hanging wall of the South Basalt fault.
在下由衷感激不尽!
最好帮我把每个单词的意识注解一下,最好不要单纯的在网上直接翻译!
谢谢! 展开
Mineralization consists of quartz veins, stockworks, veinlets, and fractures bearingmolybdenite, pyrite, magnetite, minor chalcopyrite, and rare bornite, bismuthite, galena,wulfenite, scheelite, and specularite. Quartz veins mineralized bymolybdenite occurmilky white to banded or ribboned and are often brecciated and healed by quartz and latestage calcite and minor chalcedony. Molybdenite varies in grain size from very coarse
and greasy to microscopic grains in quartz, referred toas "black quartz ore".Disseminated molybdenite mineralization occurs as broad halos around and between the veins in the Endako pit but is lacking in the Denak pits where discrete mineralized veins and narrow low grade envelopes are separated by waste (Figure 7-3). Individual quartzmolybdenite veins have limited extent; however, the vein systems in which they occur can be traced throughout the deposit (Bysouth and Wong, 1995).The pyrite zone lies to the south of and adjacent to the orebody and has a transitional boundary in the immediate hanging wall of the South Basalt fault.
在下由衷感激不尽!
最好帮我把每个单词的意识注解一下,最好不要单纯的在网上直接翻译!
谢谢! 展开
2个回答
展开全部
成矿
成矿包括石英静脉, stockworks, veinlets, 并且破裂bearingmolybdenite, 硫铁矿, 磁铁矿, 较小黄铜矿, 并且罕见的斑铜矿, bismuthite, 方铅矿,wulfenite, 白钨矿, 并且specularite。石英成脉络矿化的bymolybdenite occurmilky白色对结合或经常ribboned并且是brecciated和由石英和latestage方解石和较小玉髓愈合。 辉钼矿在粒度在石英变化从非常粗糙和油腻对微观五谷, 被提到的toas “黑石英矿石”。传播的辉钼矿成矿在Denak坑在Endako坑发生作为宽广的光晕在和在静脉之间附近,但缺乏,分离矿化的静脉和狭窄的低档信封由废物(图7-3)分离。 各自的quartzmolybdenite静脉限制了程度; 然而, 他们发生的静脉系统可以被追踪在储蓄中(Bysouth和Wong, 1995).硫铁矿区域对和在矿石藏量附近南部在并且有一个过渡界限在南玄武岩缺点的直接上盘。
成矿包括石英静脉, stockworks, veinlets, 并且破裂bearingmolybdenite, 硫铁矿, 磁铁矿, 较小黄铜矿, 并且罕见的斑铜矿, bismuthite, 方铅矿,wulfenite, 白钨矿, 并且specularite。石英成脉络矿化的bymolybdenite occurmilky白色对结合或经常ribboned并且是brecciated和由石英和latestage方解石和较小玉髓愈合。 辉钼矿在粒度在石英变化从非常粗糙和油腻对微观五谷, 被提到的toas “黑石英矿石”。传播的辉钼矿成矿在Denak坑在Endako坑发生作为宽广的光晕在和在静脉之间附近,但缺乏,分离矿化的静脉和狭窄的低档信封由废物(图7-3)分离。 各自的quartzmolybdenite静脉限制了程度; 然而, 他们发生的静脉系统可以被追踪在储蓄中(Bysouth和Wong, 1995).硫铁矿区域对和在矿石藏量附近南部在并且有一个过渡界限在南玄武岩缺点的直接上盘。
参考资料: http://tran.httpcn.com/trannew.html
已赞过
已踩过<
评论
收起
你对这个回答的评价是?
2006-10-13
展开全部
矿化
矿化有石英血管, stockworks , veinlets 和破碎 bearingmolybdenite ,黄铁矿, 磁铁矿,较小的黄铜矿和稀有的斑铜矿, bismuthite ,方铅镀, wulfenite ,重石和 specularite。 石英血管矿物化 bymolybdenite occurmilky 白色联合或者用丝带装饰和 brecciated 时常是而且痊愈被石英和 latestage 方解石和较小的玉髓。 辉铜矿在谷粒大小方面改变从非常粗糙的
而且油腻的对石英的显微镜的谷粒, 提到 toas\" 黑色的石英矿石 \".散播辉铜矿矿化在附近和在 Endako 深坑中在血管之间发生如宽广的晕轮但是正在缺乏 Denak 坑哪里不连续的矿物化血管和信封被废物 (图 7-3) 分开的狭窄部份低点等级. 个别的 quartzmolybdenite 血管已经限制范围; 然而, 血管制度在哪一个他们发生能在存款各处被追踪.(Bysouth 和 Wong,1995)对南方的黄铁矿地域谎言和与 orebody相邻而且在南玄武岩过失的立即的悬挂墙壁中有变迁的边界。
矿化有石英血管, stockworks , veinlets 和破碎 bearingmolybdenite ,黄铁矿, 磁铁矿,较小的黄铜矿和稀有的斑铜矿, bismuthite ,方铅镀, wulfenite ,重石和 specularite。 石英血管矿物化 bymolybdenite occurmilky 白色联合或者用丝带装饰和 brecciated 时常是而且痊愈被石英和 latestage 方解石和较小的玉髓。 辉铜矿在谷粒大小方面改变从非常粗糙的
而且油腻的对石英的显微镜的谷粒, 提到 toas\" 黑色的石英矿石 \".散播辉铜矿矿化在附近和在 Endako 深坑中在血管之间发生如宽广的晕轮但是正在缺乏 Denak 坑哪里不连续的矿物化血管和信封被废物 (图 7-3) 分开的狭窄部份低点等级. 个别的 quartzmolybdenite 血管已经限制范围; 然而, 血管制度在哪一个他们发生能在存款各处被追踪.(Bysouth 和 Wong,1995)对南方的黄铁矿地域谎言和与 orebody相邻而且在南玄武岩过失的立即的悬挂墙壁中有变迁的边界。
已赞过
已踩过<
评论
收起
你对这个回答的评价是?
推荐律师服务:
若未解决您的问题,请您详细描述您的问题,通过百度律临进行免费专业咨询