常用岩芯描述英词汇及简写.docx
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常用岩芯描述英词汇及简写
常用岩芯描述英语词汇及简写
coordinate co 一致BuAzO>=
coordinate ord 座标dR>$vbjh1Z
coordinate ord 一致J^DyhCs
coquina coq 贝壳灰岩e{4ecoral crl 珊瑚DH$Nz
coralline corln 珊瑚的tNqSCjQ~_c
coralline corln 珊瑚状&F;bg
core c,- 岩心e?
?
h^
corehole CH 取心井EN}4-P/5
corrected corr 校正好的tK+JmbB\
correcteddepth CD 校正井深d}?
KPJ{
correlate correl 对比FSkX95
cover cov 覆盖层tk5p@l
cover cov 包括AEFd,;GF
cream crm 淡黄色I&^hG\D
cream crm 奶油色EuVA"~PA
crenulate cren 细褶皱CNWA!
1n^Hy
crenulate cren 锯齿状HB<>x
cretaceous K 白垩系5lwMc0{/3
cretaceous K 白垩纪N/;Vg^Wx
cretaceous Cret 白垩系Lo）T
cretaceous Cret 白垩纪QPFv]^s（
crevice crev 裂隙nF,zWr[x
crinkled crnk 褶卷曲i8*（J-M
crinkled crnk 成波状NXS$w{^
crinoid crin 海百合z'5
cross X 交错!
bX
cross-laminated Xlam 交错纹层wH`GzB"
cross-stratified Xstrat 交错层理$>wN:
uN（
crossbed Xbd 交错层`0W+（9}
crossbeding Xbdg 交错层理（r1"!
~d@
crumbly crmb 易碎的w[^lxq
crumbly crmb 脆的S}&1_I
crumpled crpld 挤压$?
O
Qtz@
crumpled crpld 变皱{{1qkG9$
crumpled crpld 扭曲H<*n5r（c
crypto crp 隐8K\S]SZ
crypto crp 隐蔽~KxK+6[:
cryptoprefix crp 隐uPb.uG
cryptoprefix crp 隐蔽"（p&Oz
cryptocrystalline crpxl 隐晶质的IL%P\Zs
cryptofissile crpfiss ,Mn`kLcryptograined crpgr 隐晶岩?
{OU%usQwE
crystal xl 晶体{@t6[g++
crystal xl 结晶aM\Ph&c7e'
crystalline xln 晶质的-]:
1zU
crystalline xln 结晶的A-u}&}l<
cube cub 立方的h-%RSei5
cube cub 立方体`bNLmTS
cubic cub 立方的+"VXw2R_e
cubic cub 立方的&M#}?
@!
C
cubicfoot CF 立方英寸HQc^ybX5
cummulative cum 累计的[h0）V（1KR
cut ct 切TcH7!
fUj
cut ct 割9gETWz（3I
cut ct 馏点
if+97^Oy
cutflourescence CF 溶液荧光mzn#4;m$
cutting ctg 切割vgKdhN2kI
cutting ctg 切片P5Pb2|\*
cuttings ctgs 岩屑X>Y>1fI.
cuttings ctgs 钻屑cycle cyc 旋回%"AB\l
L.
cycle cyc 周期;x-]1xx_
cycleperminute CPM 转/分）8V=!
73
dacite dac 英安岩]=（P
tzVa
dark dk 暗的J|DY/v
dark dk 深的\s,~|0_V
darker dkr 暗的F;Bq[V）R
darker dkr 深的M）sAMfuUw
debris deb 岩屑1F{,Zr
debris deb 碎石k6（0:
/C
decrease decr 减少T}Ve:
S
decrease decr 降低r）[Xzn
degree deg 度y*#+:
D]o*
degree deg 程度REJHh\:
.77
degree deg 方次h.5KzCS
dendritic dend 树枝的3shd0q<
dendritic dend 多枝的\qtdbi|Y
dense dns 浓的0t6DD
dense dns 稠密的Pdk#"H-j
dense dns 密集的F[]6U/gn
density dnsty 密度"&@{f:
+
depositional depstnl 沉积的@]dv
depositional depstnl 沉积作用的lg*?
w/JX+
depthunit DU 深度单位|2Uw8M7.E
description des 描述X~Hm.qIR
description des 说明4mnVXKt%.
dessication des 干躁剂.pIOdetermine dtrm 确定d2Ta&Md
determine dtrm 决定C=JS]2W2
determine dtrm 限定.TNGi
UzG
detrital dtrl 碎屑的u@t~*E5BpM
detritus dtrs 碎石8L5O5F'
development dev 发展u-*z#e_L0
development dev 开发JA4}Bwn
deviation dev 偏的`W.g1"o8W4
deviation dev 偏差[}dPn61
devonian D 泥盆系3AAciMq}
devonian D 泥盆纪Y$s4*）%
devonian devo 泥盆系OxUc,%e9P
devonian devo 泥盆纪NDJP`FI
diabase db 辉绿岩eKf5orN
diagenesis diag 成岩作用1fC）&4W
diagonal diag 斜的NMUF）ksjN
diagonal diag 对角线的1hD（l6tG@
diameter dia 直径O%w'nz"
diametor dia 直径的%evtIUdiametor diam 直径的P）LOAe1'
diamictite diamic 杂岩t+\diamictite diamic 混杂陆源沉积岩j8aH*K-l{
siffierent dif 差异+R~!
G
siffierent dif 区别$wDSED-
siffierent dif 不同*9aI\#}
diorite dr /1$u|Gs*
dirty drty 泥土f1sp6S0V\
discontinuous discont 不连续的Mpco8b-b
dolomite dol 白云石fjY:
u,5V_
dolerite do 粗粒玄武岩v`G}sgn
dolerite do 辉绿岩]7oo`KcQ|
dolomitic dolc 白云石的b80&
${v
dolomitized dold 白云岩化}E[vW
dolomold dolmd 白云石穴hpYv*WH:
dolomold dolmd 白云石晶模IKaW],sr#
dolostone dolst 白云灰岩jeJspch+#
dominant dom 主要的R3.w"）6
dominant dom 占优势的l*h
uKSX}
druse drs 晶族Bj9FSKiH
druse drs 晶洞BwGOn）KL
drusy drsy 晶族状>n（dyU@
dusky dky 微暗的b?
VByJl
maximumdipangle DMAX 最大倾角uFhPNR2l
normalcalculatedDexponent DCN 正常D指数（FZ8T39
earthy erthy 土状的fe"w--v
earthy erthy 泥土的0pl'*r*9
echinoidal ech 海胆类p!
）tA
effectivecoreporosity ECP 岩心有效孔隙度^,?
>6O
elevation elev 海拔高度Z#[%JUYp'
elliptical elip 椭圆形的n"^rS}Y]
elongate elg 伸长状*CAz_s<
elongate elg 狭长状k.Gt}\6zP
embedded embd 埋入的;~WoJlEK3
embedded embd 嵌入的,?
Vxcr
eocene Eoc 始新世kK5~hpv
equivalentcirulatingdensity E.C.D 等效循环密度4`cfFowK~
equivalentmudweight E,M.W 当量泥浆必重0"+QWh
eroded erod 侵蚀的verosional eros 冲蚀vl|3WYA
erosional eros 侵蚀estimated est 估计d~QJ}a
estimated est 评价Y2N$&]O{
estimated est 判断YY'[PXP$Y
euhedral euhed 自形的_n4`mL8>kH
euxinic eux 静海相的I>-}ys`[
euxinic eux 闭塞环境Ml+f3#HP
evaporite evap 蒸发岩40-/t*2Ly
evaporite evap 蒸发盐-ucR@P]
example ex 例子6jl{^dI
excellent excel 优良的*1>Tc,mb
excellent excel 极好的kll,^A
exposed exp 暴露的`0{q
fms
externalupsetend EUE 外加厚n4ti{-^4|d
extraclast exclas 外来碎屑~extraclastic exclas 外来碎屑G0ENk|wbbj
extremely extr 极度$,T3vX]<
extremely extr 极端er!
+QD,EM
extremely extr 终极\l3M\$oS>
fabric fab 结构!
|Y&h0e
fabric fab 构造m（WVxVB
facet fac 磨光面1+Y;"tT
facet fac 刻面lt}U,p,S
faint fnt 微弱的.MRLAG
faint fnt 淡的OL#RkD
fair fr 好的e?
-LB
fair fr 公正\G1（r=fU
fault flt 断层Xc]Q_70O
feet ft 英尺rB5+~K@
feldspar fld 长石~bJ*LM?
wOP
fenestra fen 模孔woK?
td|/
fenestra fen 窗孔.w]S!
=h
ferro-mag fe-mag 铁锰铜和金NW;wy;;
ferruginous ferr 含铁的mdHC{sp
ferruginous ferr 铁质6T~xjAuJ3T
few fw 少量9Uhnr]J.
fibrous fibr 纤维状x;*KRO
fibrous fibr 纤维质1{S"axSL
fill fl 冲填:
!
Tb/1
filtercake FC 泥饼VIxcyp0X
fine f 细"2bCq]I0
fine f 细粒的w
~g）Dz2G
fine f 好的g<{jgF
firm frm 硬<[7.+{qfW
firm frm 坚硬VscEdtkd
fissible fis 裂变物质I.\fhNxHY
fissible fis 易剥裂的y8un&LP
flagofshale FSHA 泥岩标志X}xyv
flaggy flg 断层{@oYM
O~
flaggy flg 薄层\qqt/
flake flk 薄片><[（$Gq`g
flake flk 磷片kfB
VF%90
flat fl 平的*O|Z[>
flat fl 无光泽的`Q*L!
/K+
flourescence flour 荧光
_d&FB~=
foliated fol 叶片状Qd1Q~PBla
foliated fol 薄层状>v`lsCGb
formation fm 地层QdL;|3K9
formation fm 形成mh!
;W=|/"
formation fm 建造%^gBDlR^
formationflacter FC 地层因素U&|=dH]-
fomationwater FmW 地层水_gjsAbM
fossil foss 化石utC]GiR
fossil foss 含化石的S,EXc^A7
fossiliferous foss 化石O2?
ye4uq
fossiliferous foss 含化石的
fracture frac 断口6|t4\'
fracture frac 裂缝Y（ly0U}
fracture frac 破裂b&B<'Wb
fragment frag 碎块n|Vs27
fragment frag 碎片~S15tZ$
fragment frag 碎屑i2A>T/?
{
frequent freq 频繁s={AdQ
frequent freq 经常gYfN?
A*`_
frequent freq 常见的~mxme6"v
framestone framest 骨架岩u{yENZ^P
fresh frs 新鲜的G2U=*|
fresh frs 淡的|\%[e@u
freshbreak FB 新破碎的uuHR!
freshwater Frw 淡水QpwOrxI}
friable fri 易碎的'{p/F$
friable fri 脆性的s3kHNDdC
fringe frg 边缘0m$f9b|Q?
fringe frg 条纹bO>q`%&
friosted fros 无光泽的wv>*g:
El'
good g 好0B#9CxU%
gradationalcontact grad-con 整合接触关系x.CUJ^_.
grade grd 粒级W~（@*H
grade grd 坡度'g.9goQ
grade grd 等级:
so2{.t-
gradient grad 梯度（|+Sbq（o
grading grdg 分选oU`8\n]（
grading grdg 分级qniP`P4E
grain gr 粒I,;@\
grain gr 颗粒.XDY1~w0
gradual grad 逐渐的l3kYfq{";"
grainstone grst 粒状灰岩X,-QxV=lc）
grainstone grst 颗粒岩aDEz|>q
gram/liter g/l 克/升Z3jh-{0
granite grnt 花岗岩rHe*/nN%*
granitewash grntw 花岗冲积物Pf,S`Uw;
granitewash GW 花岗冲积物iT*!
3
granitic grntc 花岗岩的xW|^2k
grano-diorite grndior 花岗闪长岩X^204K%:
granodiorite grndior 花岗闪长岩!
C}t）R]^
granule gran 细粒85;hs
granule gran 粒砂3Ee8_（E\
granulestone granlst 细粒aJh=4j~.
granulestone granlst 颗粒岩7\.Ax
grapestone grap 笔石mX
@Un9k
grapestone grnpst 葡萄状灰岩@\~qXz{6J
graptolite grap 笔石WW.\5kBl8
gravel gvl 砾石@（:
ah
gravel gvl 砂砾WZ.d"EE"
gravity grav 重力U3ygFW%
gravity grav 比重>.R6\>N%
gray gy 灰色2>{_O?
UN
greasy gsy 油性的Kuh!
b`9
greasy gsy 多脂的niO（>
green gn 绿色的qA-ya6
greywacke gywk 杂砂岩my#qmI
greywacke gywk 硬砂岩C9-9cdWH
grit gt 粗砂质的-_jV.`t
gritty gt 粗砂质的$,kSR}
groovecast grvcst 凹槽#
（nheL
ground grd 地面!
2x"'o
groundlevel GL 地平面x7e
groundlevel GL 地平线;U<）$5
group G 团体gb:
Cc,F,%
gummy gmy 胶质w8%yX$<
gummy gmy 粘性+!
POKr
gypsiferous gyp 含石膏:
0T]p"y4
gypsum gyp 石膏^J>28Q\S
hackly hkl 锯齿状>1ZMQgCG
hackly hkl
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