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palaeokarst
古岩溶
常用释义
词性释义
古岩溶
例句
全部
The
well
developed
palaeokarst
feature
in it
is
due
to
multistage
tectonic movement
and
its
intrinsic
sedimentary
characteristics
.
由于多期构造运动及沉积体系自身的特征使古岩溶十分发育。
So the
research
findings
will
provide
reliable
evidence
for
the
palaeokarst
reservoirs
evaluation
and
favorable
area
optimization
.
上述研究成果将为川东石炭系古岩溶型储层评价与有利区带优选提供可靠依据。
Many
reverse
faults
develop
in
Ordovician
palaeokarst
in
Tahe
region
,
which include
mainly
NW
,
and
NE
,
and
EW
,
and
SN
directional
.
塔河地区奥陶系发育加里东中期、加里东晚期—海西早期和海西晚期的逆断裂，断裂走向总体为NW向、NE向、EW向和SN向为主。
Hercynian
palaeokarst
slope
and
palaeokarst
upland
are
favourable
to the
development
of
karst
pores
.
海西期古岩溶斜坡带和古岩溶高地是岩溶空隙发育的有利区。
The
Ordovician
palaeokarst
had gone
through
3
evolution
stages
and
there are
7
types
of
developed
patterns
in
the
Huanghua
Depression
.
黄骅坳陷奥陶系古岩溶经历了3个演化阶段，具有7种发育模式。
Palaeokarst
Characteristics
and
Controlling
Factors
of
Marine
Carbonate
Rocks
in
Jianghan
Plain
and
its
Neighboring
Areas
江汉平原及邻区海相碳酸盐岩的古岩溶特征及控制因素
Indication
of
Mineral
Inclusion
Characteristics
to
Palaeokarst
Actions
矿物包裹体特征对古岩溶作用的指示性
Application
of
Seismic
Physical
Forward
Modeling
in
Palaeokarst
Reservoir
Study
地震物理正演模拟在古岩溶储层研究中的应用
Restoration
of
Pre
-
Carboniferous
Palaeokarst
Landform
in
Central
Ordos
Basin
鄂尔多斯盆地中部前石炭纪岩溶古地貌恢复
Controlling
Effects
of
Fault
over Ordovician
Palaeokarst
in
Tahe
Region
塔河地区断裂对奥陶系古岩溶的控制作用