glacial maximum 中文意思是什麼
glacial maximum
解釋
冰川極盛期；最大冰河期-
Variations in the eolian environment of north america during the last glacial maximum and their signifi cance in the global abrupt climatic events
末次盛冰期北美風成環境變化及其在全球氣候突變事件中的意義 -
As a result of the sea - level drop at the last glacial maximum in the late quaternary, the distribution of the land and sea in the eastern china continent changed a lot
第四紀晚期，由於末次冰期的出現，中國大陸東部海陸分佈發生重大變化。 -
The provenance of the sediment in middle okinawa trough during the last glacial maximum is the shelf of the east china sea. the characteristics of elemental geochemistry ascertain that the sediment was derived from the paleo - changjiang river
末次盛冰期沖繩海槽中部陸源物質來源於東海陸架，元素地球化學特徵顯示這些沉積物主要來源於古長江的入海物質。 -
The fall of global sea level during the last glacial maximum enhanced the fluvial gradient and river cutting, resulting in the formation of the large - scale qiantangjiang river and taihu incised valleys which were subsequently filled and rapidly buried in the post - glacial period, with the paleointerfluve being exposed to air on both flanks of the incised valleys
末次冰盛期，海平面下降的幅度大，增加了河流梯度、加強了下切作用，形成了錢塘江和太湖下切河谷，隨后在冰後期被充填和埋藏，下切河谷的兩側為暴露地表的古河間地。 -
Comparison of the characteristic parameters of immobile elements, such as ree, sc, th, ti etc and of the characteristics of sedimentology and mineralogy comes to a conclusion that the provenance of the sediment is different in the last glacial maximum and in the sub - interglacial stage, and they have the traits of mixed source. during the last glacial maximum the sediment in the outshelf of the southern east china sea was affected weakly by changjiang river and they are probably derived from the coast mountains of zhejiang - fujian province, which are near the southern east china sea
通過對東海外陸架樣品的稀土元素和sc ， th ， ti等不活潑元素地球化學物源示蹤指標對比，再結合沉積學和礦物學特徵，判斷末次盛冰期與盛冰期以前的沉積物具有不同的物質來源，不同時期的沉積物都具有混合物源的性質，盛冰期東海南部外陸架沉積物受長江物源影響較小，可能來源於距東海南部較近的浙閩沿海山地。 -
The contribution of the glacial meltwater accounted for about 74 %, and that of moraine - dammed lake outburst accounted for only 26 % of the maximum discharge
這是一種多因子共同作用的新型泥石流類型，不同於以往的冰川融水型泥石流和冰湖潰決型泥石流。
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