fine sediments 中文意思是什麼
fine sediments
解釋
細泥沙-
In such fine sediments, cohesion is an important factor in determining critical conditions.
在這樣的細沙中，粘性是確定臨界條件的一個重要因素。 -
The time corresponding to the four parts along the section are as follows : the top lake - swamp sediments : holocene ; the uppart fine sand : later late pleistocene ; the middlepart sandy clay : middle - early late pleistocene ; the lowpart clayer silt : later - middle - pleistocene. the fossils and stone artifacts found in salawusu site should be formed during the last but one glacier, its age range is about 0. 13 - 0. 19 ma, and belongs to later middle - pleistocene
分析q曲線與氧同位素曲線的一致性以及以上研究結果，包含薩拉烏蘇地層的這套沉積物的沉積時代為：頂部湖沼相沉積物：全新世；上部具交錯層理的細砂：晚更新世晚期；中部粉砂質粘土：晚更新世中期至早期；下部粘土質粉砂：中更新世晚期。 -
The ore - hosting yaojia formation is composed of a set of braided stream medium - fine grained sediments
摘要姚家組為一套中細粒辮狀河流沉積。 -
Water body is shallow and sediments are coarse in lst and hst, but in tst, being deep and fine
低水位體系域和高水位體系域水體較淺，沉積較粗，而湖進水位域則水體較深，沉積較細。 -
The palaeogeographic research indicate that the palaeogeographic outline of the study area recorded the evolution from a sedimentary basin in which the shallow - water carbonate platform sediments and deep - water terrigenous clastic submarine fan developed from southeast to northwest and northeast during the late triassic through a submarine sheet - like model composed of deep - water sandy turbidite and fine - grained turbidite during the early jurassic to a terrigenous clastic barrier coast during the middle and late jurassic and finally to the coal - bearing delta sediments during the late cretaceous
古地理分析表明，研究區晚三疊世古地理輪廓是一個從東南向西北和東北方向由淺水碳酸鹽臺地及深水陸層海底扇沉積共同發育的沉積盆地；早中侏羅世，演變成為一個由深水砂質濁積巖和細屑濁積巖組成的水下席狀體沉積；進入中晚侏羅世，其古地理表現為一個陸屑淺海有障壁海岸；到了晚白堊世，研究區表現為以含煤沉積為特徵的三角洲相沉積。 -
Effects of alcl3, mgcl2, cacl2 and humus on the flocculation of fine sediments in the high - turbid system of the changjiang estuary
2和腐殖酸對高濁度體系細顆粒泥沙絮凝的影響 -
The element content in the fine - grained fraction ( < 0. 063mm ) of the core is great. the correlation coefficient between the elements in the coarse - grained is high, which indicate that the coarse - grained sediments derived from the same provenance
柱樣中細粒級（ 0 . 063mm ）元素含量較粗粒級（ 0 . 063mm ）高，變化幅度大，從元素之間相關性來看，粗粒級的元素之間相關系數高，表明粗粒級物質具有統一來源。 -
Polygonal fault is a type of non - tectonic fault distributing in deepwater fine - grained sediments
摘要多邊形斷層為一類非構造斷層，主要分佈於深水環境下的細粒沈積物中。
分享友人