1.
Dandruff consists of scaly particles with an oily sheen that lie close to the hair root. This condition should not be confused with a flaky scalp .
头皮屑是由油光发亮的鳞状颗粒组成,附着在头发根部,请勿将此与头皮碎屑相混淆
2.
Dandruff consists of scaly particles with an oily sheen that lie close to the hair root. This condition should not be confused with a flaky scalp (see below).
头皮屑是由油光发亮的鳞状颗粒组成，附着在头发根部，请勿将此与头皮碎屑相混淆（见下）。
3.
Transition from marine clastic rocks to nonmarine clastic rocks in the west of Sichuan Basin,China
四川盆地西部海相碎屑岩-陆相碎屑岩的转换过程
4.
MICROFACIES MARKERS OF CLASTICS OF THE LOWER TERTIARY IN JIYANG SAG
济阳坳陷下第三系碎屑岩微观相标志
5.
sparry intraclastic calcarenite
亮晶内碎屑砂屑灰岩
6.
The sediments are detrital and largely of greywacke facies.
沉积岩为碎屑质，大部分属于杂质砂岩相。
7.
Clastic facies pattern recognition is somewhat systematic.
碎屑岩相模式的识别是带有一定系统性的。
8.
Lower Carboniferous is composed of sea facies fragments and mid-acidic component igneous rock.
下石炭统为海相碎屑岩及中酸性岩组合 ;
9.
In lithology, the calcareous sandstone is of coarse grain and fairly well sorted.
岩性主要为粒度相对较粗、分选较好的碎屑岩。
10.
grated pineapple
菠萝米, 菠萝碎(屑)
11.
5. the lagoon and swamp.
5)泻湖和沼泽相——位于两道平行砂堤间,由生物碎屑和陆源碎屑堆积而成。
12.
To brush(a table or cloth) clear of small scraps or fragments of food.
抹去碎屑抹去（桌上或布上）的食物碎屑
13.
Glauconite, detrital carbonate skeletal debris, marine fossils, and collophane are commonly present.
海绿石、碳酸盐骨骸碎屑、海相化石和胶磷矿普遍出现。
14.
THE CHARACTERISTICS AND GENETIC SIGNIFICANCES OF PROBABILITY ACCUMULATION CURVES OF DEVONIAN MARINE VOLCANOCLASTIC ROCKS IN EAST ZHUNGEER
东准噶尔泥盆系海相火山碎屑岩概率累积曲线特征及其成因意义
15.
1. There was a terrestrial facies lake basin in study area and mainly developed clastic rock during the late Trias.
1、研究区晚三叠系为陆相湖盆沉积，以发育陆源碎屑岩系为主。
16.
Characteristics and evaluation of Mesozoic and Cenozoic clastic reservoirs in the Tabei Uplift
塔北隆起中、新生界陆相碎屑岩储集层特征及评价
17.
The Research of Clastic Rock Sedimentary Micro-facies and Prediction for Favorable Areas in Block of Ka 1, Tazhong
塔中地区卡1区块志留—石炭纪碎屑岩沉积微相研究及有利区预测
18.
The Late Triassic transition from marine carbonate rock to clastics in the western Sichuan Basin
四川盆地西部晚三叠世海相碳酸盐岩—碎屑岩的转换过程