英语-石油化工-勘测地质报告-地质、地矿类-石油勘探工程-高级

英语-石油化工-勘测地质报告-地质、地矿类-石油勘探工程-高级本文简介：英中句子1．Thistypeofdatadoesnotofferthedetailedresolutionavailablewithmoreexpensive“high-folddata”andtheabilitytocorrectlyinterpretsmallfaultadthinbeddipi

英语-石油化工-勘测地质报告-地质、地矿类-石油勘探工程-高级本文内容：

英中

句子

1．

This

type

of

data

does

not

offer

the

detailed

resolution

available

with

more

expensive

“high-fold

data”

and

the

ability

to

correctly

interpret

small

fault

ad

thin

bed

dip

is

hampered

by

the

poor

resolution

in

some

instances.

这种类型的数据不提供精细的分辨率，除非能提供更昂贵的“高褶皱数据”；并且，在某些情况下，数据正确解读微小ad薄层浸入错误的能力也被不良的分辨率所限制。

2.

Salt

diapirism

drives

the

deformation

and

faulting

in

the

overlying

Jurassic

and

Triassic

strata

to

form

structures

with

potential

to

trap

hydrocarbons.

盐底辟作用使侏罗纪时期的表面覆盖层和三叠纪时期的地层变形和断层，形成能储存烃类物质的结构。

段落

The

newly

available

3D

future

prospect

will

be

highly

independent

of

any

foregoing

success

or

failure.

The

newly

available

3D

seismic

surveys

represent

a

significant

advantage

over

the

2D

seismic

that

was

available

for

initial

evaluations

of

Blocks

A

and

E.

All

of

the

prospects

reviewed

have

been

mapped

using

regional

exploration

or

sparse

3D

seismic.

This

type

of

data

does

not

offer

the

detailed

resolution

available

with

more

expensive

“high-fold

data”

and

the

ability

to

correctly

interpret

small

faults

and

thin

bed

dip

is

hampered

by

the

poor

resolution

in

some

instances.

新到来的3D勘探技术不依靠之前任何的成功或者失败。新3D地震测量比只具有初步测量A区和E区的2D测量有显著优势。所有提到过的测量都已经用区域勘探或者零星三维地震被制成图。这种类型的数据不提供精细的分辨率，除非能提供更昂贵的“高褶皱数据”；并且，在某些情况下，数据正确解读微小ad薄层浸入错误的能力也被不良的分辨率所限制。

Prospects

targeting

the

pre-salt

Carboniferous

and

Devonian

strata

are

defined

primarily

by

3D

seismic

detection

of

geological

structures

below

the

highly

deformed

Kungurian

salt

sequence.

“Type

II”

prospects

are

mapped

as

structural

highs

below

the

P1

unconformity.

The

exploration

concept

is

that

these

highs

are

carbonate

buildups

analogous

to

Tengiz,Karachaganak

and

Kashagan.

RSC

concurs

that

the

deepest

Devonian

interval

(below

horizon

DEV2)

identified

by

Max

has

an

atoll-like

seismic

character

in

the

prospective

areas.

However,overlying

Carboniferous

and

Devonian

intervals(CARB

and

DEV1)

exhibit

regional

seismic

character

and

are

considered

secondary

objectives.

The

Type

II

prospects

are

about

two

kilometers

deeper

than

the

major

Paleozoic

oil

fields

in

the

region

that

Max

considers

analogous

and

are

evaluated

as

sour

gas-condensate

reservoirs.

RSC

considers

the

TYPE

II

prospects

to

be

highly

dependent

such

that

success

or

failure

at

one

could

strongly

influence

the

COS

of

the

others.

以石岩纪盐下层系和泥盆纪地层为目标的勘探，首先用3D地震探测技术，通过探测严重变形的空谷尔期地质结构盐的排列顺序进行初步定义。

“类型Ⅱ”勘探绘制P1之下形成构造隆起的不一致性。勘探理念是，这些隆起是类似于田吉兹，甘纳克和卡沙甘油田的碳酸盐沉积。RSC认同由Max鉴定出的最深的泥盆纪间隔（在地平线DEV2以下）在预定的区域有环状珊瑚岛类型的地震特征。但是，上覆盖的石炭纪和泥盆纪间隔（CARB和DEV1）展示了区域性地震特征，被认为是次要目标。类型Ⅱ勘探比主要的古生代的油田深大约2公里。Max认为该古生代的油田地区与之类似，都是酸性气凝聚层。RSC认为类型Ⅱ勘探依赖性很强，也就是说，一个地方的成功或失败将会严重影响其它的COS。

“Type

I”

pre-salt

targets

are

represented

by

the

Kuzbak

and

Akatkol

features.

These

are

interpreted

by

Max

to

be

localized

Permian

tidal

flat

or

sabka

deposits,forming

structural

highs

above

the

P1

unconformity,entirely

sealed

by

overlying

Kungurian

salt.

RSC

supports

the

Max

structural

interpretation

and

concurs

that

reservoir

quality

is

the

most

significant

risk

factor.

RSC

believes

that

the

Type

I

prospects

are

also

highly

dependent

with

respect

to

COS.

“类型Ⅰ”盐下层系靶区以Kuzbak和Akatkol特征为代表。Max解读此类特征为地区性二叠纪潮滩或盐沼沉积，在P1之上形成构造隆起的不一致性，并完全被空谷尔期盐层覆盖。RSC支持Max的构造解释，并且肯定了储层性质是最重大的风险因素。

RSC相信类型Ⅰ勘探同样高度依赖COS。

中英

句子

1.

在前期Zina区块油气勘探前景评价基础上，对新采集的二维地震资料和原有二维地震资料进行联合解释成图，结合区块内完钻的Zina-1井、Zina-2x井钻探资料，对该区块石油地质条件进行重新认识，对勘探前景进行新的评估，取得了一定进展，全面完成了合同的任务要求。

Based

on

the

earlier

stage

of

Zina

oil-gas

exploration

prospect

evaluation,the

newly

collected

2D

seismic

data

and

original

2D

seismic

data

were

interpreted

jointly

and

mapped;

The

misering

data

of

drilled

well

Zina-1,Zina-2x

were

Integrated

to

make

a

recognition

of

the

petro

geological

conditions

in

this

area.

The

exploration

prospect

was

reevaluated,certain

progress

was

made,and

the

mission

requirements

of

the

contract

were

fully

completed.

2.

类比Bongor盆地与济纳盆地的地震剖面和反射特征，济纳盆地的地震剖面上有4个不整合界面（图1-2），推测它们是基岩、下白垩统、上白垩统、古近系、新近系之间的区域不整合界面（分别对应为Tg

、T4、T3、T2）

Analogize

the

seismic

section

and

reflection

character

of

Bongor

basin

and

Zina

basin,the

seismic

sections

of

Zina

basin

are

formed

by

4

different

unconformity

interface(figure

1-2),supposedly

regional

unconformity

interface

among

bed

rock,lower

cretaceous,upper

cretaceous,palaeogene,neogene

(conrrespondly:

Tg,T4,T3,T2).

段落

平面上主要发育两组断裂体系（图2-7至图2-12）：即近东西向和北北西向断裂体系。这两组断裂交叉形成断裂网络，控制了该区的构造格局。其中近东西向的断层是济纳盆地发育的起主导作用的断裂系统，它们控制了济纳盆地的形成、构造带的形成、区域构造形态、构造类型、地层的沉积及其演化；北北西向的断裂不及北东向断裂发育，早期为共轭剪切断层，后期北西西向断层是在盆地形成过程中起调节作用的转换断层，对构造起到分割作用，控制局部构造的形成和形态。剖面上大都呈现为铲式正断层，这些断层呈“y”型、反“y”型、花状组合样式。

Plane

surface

mainly

developed

into

two

fault

systems

(Figure

2-7

to

Figure

2-12):

ie

East-West

and

North-Northwest-trending

fault

system.

These

two

systems

intersected

and

fractured

to

form

the

fracture

network,which

controlled

the

tectonic

framework

of

this

area.

Among

them,EW

faults

were

the

leading

fracture

systems

in

Zina

basin

fault

development,they

controlled

the

formation

of

Zina

basin

and

the

tectonic

zone,as

well

as

regional

structural

morphology,structural

type,stratal

deposition

and

evolution

of

Zina

basin;

NNW

fracture

was

less

developed

than

NE

faulting

which

was

conjugate

shear

faults

in

early

stage.

The

late

NWW

fault

played

a

regulatory

role

during

the

formation

of

basin;

it

split

structure

and

controlled

the

formation

of

local

structures

and

morphology.

Most

of

the

cross

sections

were

rendered

as

shovel

normal

faults;

these

faults

appeared

to

be

“y“type,anti-“y“type,and

flower-like

combination

styles.

纵向上断层分为2个级别：一级边界断层4条，控制盆地内地堑的形成和地层沉积，断距大，以南倾为主；次级别较小的同沉积断层控制局部圈闭。

Longitudinal

faults

are

divided

into

two

levels:

the

first

level

has

4

boundary

faults,which

control

the

formation

of

graben

and

sedimentary

formation

in

basin.

Fault

displacement

is

large,mainly

dumping

to

South;

secondary-level

synsedimentary

fault

with

smaller

local

traps

control

local

entrapment.

根据区域构造演化示意图（图2-6）进行断层活动的时序性分析，济纳盆地断裂的发育具有多期性。从地震剖面看，本区断裂活动主要有三期。

According

to

regional

tectonic

evolution

schematic

(Figure

2-6),time

sequence

analysis

is

made

to

fault

activities,Zina

basin

fracture

development

has

multiple

episodes

feature.

From

the

seismic

section

view,this

area

has

three

major

fault

activities.