盆口屬 的英文怎麼說
中文拼音 [pénkǒuzhǔ]
盆口屬
英文
poteriostomum-
3. it was rocky hills and relatively high in the yangtze river mouth area along changzhou, wuxi, changshu, kunshan and qingpu, which belonged to changzhou - kunshan zone according to holocene delimitation from the final stage of the liangzhu culture to the stage of the maqiao culture, due to the expansion of taihu basin and large water areas, maqioa cultural sites were concentrated on rocky hills and cheniersin the east of taihu to the west of shanghai
3 、蘇南常州、無錫、常熟、崑山和青浦一帶曾經是長江河口地區的基巖山地，在全新統地層分區上屬于常州一崑山區，是古地面地勢相對較高的地方。良渚文化末期至馬橋文化期，為太湖湖盆體系擴大時期，水域較大，所以馬橋文化遺址集中於太湖東部與上海西部地勢較高的基巖山地和砂堤之上。The ore - bearing fluid of dabaoshan deposit was relate to magmatic thermal dynamic process and formed hydrothermal sedimentary polymetallic deposit at seafloor. the ore - bearing fluid of fankou was relate to circulation hydrothermal fluid in deep formation and formed pb - zn - ag - hg polymetallic middle - lower temperature sedimentary deposit by sea - floor thermal spring overflowing
大寶山型流體與巖漿熱動力作用有關，形成海底火山熱液沉積多金屬礦床；凡口型流體與深部建造的循環熱液有關，形成中低溫海底熱泉噴溢沉積鉛鋅銀汞礦床；紅巖型流體與盆地成巖壓實水有關，形成低溫單一黃鐵礦礦床。The huachangguo gold mine bed lie in under - middle of the sanheke group of d, there has mine bend in the bike group, south of the sanheke group of d. the gold mineization is found in all crag of entire mining area, it ' s obvious pertain to the structure controlled mine, have no very much great relationship in the crag straturm
鏵廠溝金礦床產于中-下泥盆統三河口群中，南部的碧口群亦有礦化帶的存在。金礦化遍布整個礦區所有的巖性層，明顯屬于構造控礦，與所處的巖性層沒有太大的關系。The study of neogene calcareous nannofossils from the pearl river mouth basin in the last two decades could be subdivided into two stages ( 1 ) from the beginning period of the 80 ' s to early of the last century, the studies focused on the calcareous nannofossil zones and the descriptions of main genera and species ; ( 2 ) from the middle and late period of the 90 ' s of the last century to the present, the researches concentrated on the high - resolution calcareous nannnofossil biostratigraphy
縱觀二十多年來珠江口盆地新近系鈣質超微化石的研究歷史，大致可分成兩個階段： （ 1 ）上世紀80年代初至90年代初，側重於化石帶的報道及主要化石屬種的描述； （ 2 ）上世紀90年代中後期至今，主要為高解析度鈣質超微生物地層研究階段。分享友人