白雪巖 的英文怎麼說
中文拼音 [báixuěyán]
白雪巖
英文
dolomitite-
Up at sea level, the dry wash cuts through the yellowish mud - stone and siltstone for which the canyon is named, this is the place you want to see in late afternoon just hour before sundown, the hills are glowing at 24 carats. a drive to zabrishie point for fine views of the valley
站在巖面扭曲起皺顏色，或紅或紫或黑的火山巖的危崖絕壁上，看各式古代大湖乾涸后，留下來厚達兩千尺白雪狀的鹽土層，實在覺得人在時光中的渺小。Set off to five great chain lakes by bus, have lunch after arriving, visit old - aged volcanic lava volcano : underground ice river, snow world, frost flowers, ice and snow art, enjoy the winter in summer ; ice cave ( appreciate ice crystal, ice art, ice light ) ; visit famous cold spring : long life garden ( springs, mineral spring shower, sun shower, wild animals, spring square, etc. ), yishen garden ( yishen pavilion drinking spring, go fishing, go boating, see butterflies, lilac garden, etc
早乘車赴五大連池，抵達后午餐，游覽老期火山熔巖洞：地下冰河：參觀白雪世界，熔巖洞內欣賞霜花，冰雪雕，體驗夏季里的冬天；冰洞（盛夏時節，地下熔巖洞欣賞冰晶奇觀，冰雕，冰燈） ；游覽世界著名冷礦泉：長壽園（世界名泉、神泉舊址、棄石丟病、礦泉浴場、日光浴場、花卉濕地、野生動物展示園、泉之韻廣場等） 、益身園（玄武巖牌樓、益身亭、北飲泉、長廊、藥泉湖垂釣、北苑賞葦、熔巖臺地、泉湖蕩舟、泉湖浴場、火山絕蝶棲息地、丁香園等） 。Alkali basite, which came from upper mantle or lower crust, invaded through those structure, which not only bring cu et al mineralizing elements, but also the most important is that thermal energy. it cycled the formation water ( yinmin fonnation and luoxue formation ), and form alkali - rich, middle - high temperature and salinity fluid mixed with alkali - rich magmatic water. there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks, which is in favor of the transposition and mineralization of minerogenetic fluids
因此，總結東川稀礦山式銅礦成礦模式為沉積（ fe 、 cu ） ?熱液疊加（ cu ）改造：晉寧-澄江期，小江深大斷裂發生走滑運動，在東川礦區造成右行旋扭及其派生構造，形成「 z 」字形落因破碎帶，同時來自深源（下地殼或上地幔）堿基性巖漿侵入，不僅帶來了大量cu等成礦物質，更重要的是提供了熱源，促使地層水（落雪組白雲巖和因民組紫色層）循環，與富堿（ na和k ）巖漿水混合，形成富堿中高溫高鹽度流體。The following new knowledge are acquired : a ) the cu background of stratum and jinningian alkali basite is abnormal high, which could be liberated from those rocks during alteration. cu et al. minerogenetic elements, which main came from magmatic rock, some from stratum ( yinmin formation and luoxue formation ) and its basement rocks
礦床中cu等成礦物質來源復雜，以深源為主，部分來源於地層（因民組紫色層和落雪組白雲巖）及基底地層；礦區內的退色蝕變作用可能是混合流體堿質交代改造作用的結果，對銅礦形成影響明顯，是銅礦化的標志； 2A single shoot carried a considerable stream over the face of a black rock, which contrasted strongly in colour with the white foam.
一股急流在黑色的巖石上奔來，雪白的飛沫同巖石的顏色形成鮮明的對照。The sightseeing routs through diqing can be divided between those of the east and those of the west. the eastern route starting from the town of tiger - leaping gorge, to the nature reserve of haba snow - capped mountain, to the white water platform ( where one can appreciate naxi culture and dongba folklore ), to bita lake, and then to shudu lake, followed by a trip to xiagei hot springs, and after that to the natural bridge and dabao temple, and finally to the songzanlin temple
由虎跳峽鎮、哈巴雪山自然保護區、白水臺（納西風情、東巴文化游覽） 、碧塔海、屬都湖、下給溫泉、天生橋、大寶寺至松贊林寺；另一路由虎跳峽鎮、十二欄桿及其摩巖詩、千湖山、木天王城遺址、碧沽天池，仙人洞、五風山至藏經堂。This scenic area includes such places such as haba snow - capped mountain ( a provincial - level nature reserve about 153 km from zhongdian ), white water platform ( 101 km ), the zha ri cliff paintings, and longwangbian ( 150 km )
包括哈巴雪山省級自然保護區（離中甸160公里） 、白水臺（ 101公里） 、渣日巖畫、龍王邊（ 150公里）以及納西風情、東巴文化。Based on the geological, stratigraphic and geochemical characteristics of the ophiolitic melange, island - arc and rift volcanic rocks from the jinshajiang zone, an archipelagic tectonic model with multi - rift and multi - subduction is proposed to explain the evolution of jinshajiang paleo - tethys. the ophiolitic melanges of the jinshajiang zone are mainly outcropped at baimangxueshan, tongduo, gongka, dongzhulin and jiyidu in the deqin county. the geochemistry of major and trace elements of the jinshajiang ophiolite shows its geochemical characteristics are similar to those of the more and island - arc volcanic rocks, but different from those of the typical n - mopjb
金沙江蛇綠混雜巖主要分佈在德欽縣的白茫雪山、通多、共卡、東竹林和吉義獨地區，主量和微量元素地球化學特徵研究表明，金沙江蛇綠巖不具有典型n - morb的地球化學特徵，而具有介於morb和島弧之間的地球化學特徵，暗示它並非形成於寬闊的大洋環境，不是古特提斯在滇西北地區的主縫合帶，可能是古特提斯多島洋體系中的一個弧后盆地。分享友人