Most geologists think 86. that the chemical composition of the mantle rock is about the same throughout the mantle

Một phần của tài liệu Luận án tiến sĩ Ngôn ngữ học: Nghiên cứu cấu trúc và ngữ nghĩa các giáo trình địa chất như một thể loại trong tiếng Anh và tiếng Việt (Phần 2) (Trang 83 - 92)

Most think that | the chemical is about the same

geologists composition throughout the mantle.

of the mantle rock

eye Pro: . Pro: .

Transitivity Senser Carrier . Attribute mental relational

Sub. 1 Fin | Pre Sub. 2 Fin | Pre Complement

Mood Mood. 1 Residue. Mood. 2 Residue. 2

Theme

Theme (unmarked) Rheme

87. Because pressure increases with depth into Earth,

Because pressure increases with depth into Earth,

Transitivity Existent Pro: : Cir. 1 Cir. 2existential Subject | Fin Pre Adj. 1 Adj. 2

Mood Mood Residue

Theme Theme (unmarked) Rheme

88. the boundaries between mantle layers possibly represent depths at which pressure collapses the internal structure of certain minerals into denser minerals.

the boundaries | possibly | repres | depths at which pressure collapses the between mantle ent internal structure of certain minerals layers into denser minerals.

Pro:

Transitivity Sayer Cir. verba Verbiage

|

F P

Mood Subject Adj. in| 7 Complement

e

214

Mood Residue

Theme Theme

(unmarked) Rheme

89. For example, at a pressure equivalent to a depth of about 670 kilometers, the mineral olivine should collapse into the denser structure of the mineral perovskite.

For at a pressure the should | collapse into the example, | equivalent to mineral olivine denser

a depth of structure of about 670 the mineral

kilometers, perovskite

Transitivity Circumstane Actor Pro: material Goal

Adjunct Subject Fin Pre Comp! emen

Mood Mood Residue Theme

Theme (marked) Rheme

90. If the boundaries between mantle layers represent pressure-caused transformations of minerals, 91. the entire mantle may have the same chemical composition throughout, although not the same mineral composition.

If the represent pressure- the may | have |_ the same boundaries caused entire chemical

between transformations | mantle compositio

mantle of minerals, n

layers throughout, although

not the

same

mineral compositio

n

tyes Pro: . . Pro: Attribute

Transitivity Sayer verbal Verbiage Carrier relational

Mood Sub. 1 Fin | Pre Comp. 1 Sub. 2 | Fin | Pre | Comp. 2 Mood. 1 Residue. 1 Mood. 2 Residue. 2

Theme (marke 4) Rheme

92. However, some geologists think 93. that the 670-kilometer boundary represents a chemical change as well as a physical change

However, some think that | the 670 represents a chemical change

215

geologists kilometer as well as a physical boundary change

Pro: Pro: .

Tran Senser mental Sayer verbal Verbiage

Sub.1_ | Fin | Pre Sub. 2 | Fin | Pre Complement

Mood Residue. :

Mood. 1 1 Mood. 2 Residue. 2 Theme

Theme (marked) Rheme 1

94. and separates the upper mantle from the chemically different Jower mantle below.

and separates the upper from the chemically

mantle different lower mantle below.

Transitivity Pro: Goal Circumstancematerial

Ein | Pre | Complement Adjunct

Mood Mood Residue

Theme Rheme 2

The Core

95. Seismic-wave data provide the primary evidence for the existence of the core of Earth. . (See chapter 16 for a discussion of seismic P and S waves.)

Seismic- provide the primary evidence

wave data for the existence of the core of Earth

Transitivity Carrier Pro: relational Attribute Subject Fin Pre Complement

Mood Mood Residue

Theme

Theme (unmarked) Rheme

96. Seismic waves do not reach certain areas on the opposite side of Earth from a large earthquake.

Seismic do not reach certain on the opposite side of Earth

waves areas from a large earthquake.

Transitivity Actor Pro: material Goal Circumstance Subject Fin Pre Comp. Adjunct

Mood Mood Residue

Theme

Theme (unmarked) Rheme

97. Figure 17.8 shows 98. how seismic P waves spread out from a quake until, at 103° of arc (11,500 km) from the epicenter,

Figure 17.8 show how

seismic P

waves

spread

out

from a quake until, at 103° of arc (11,500 km)

from the epicenter

216

Transitivity Sayer Pro: verbal Actor Pro: Cir.material

Sub.1 Fin Pre Sub. 2 | Fin | Pre Adj.

Mood Mood. 1 Residue. Mood. 2 Residue. 2

Theme

Theme (unmarked) Rheme

99. they suddenly disappear from seismograms.

they suddenly disappear from seimograms Transitivity Actor Cir. 1 Pro: material Cir. 2

Subject Adj. 1 Fin Pre Adj. 2

Mood Mood : Mood

Residue Theme

Theme (unmarked) Rheme

100. At more than 142°(15,500 km) from the epicenter, P waves reappear on seismograms.

At more than 142° P waves reappear on seismograms.

(15,500km) from the

epicenter,

Transitivity Circumstance. 1 Actor | Pro: material Circumstance. 2

Adjunct. 1 Subject | Fin Pre Adjunct. 2 Mood Mood

Residue

Theme Theme (marked) Rheme

101. The region between 103° and 142°, which lacks P waves, is called the P-wave shadow zone

The region between 103° and 142°, is called the P- wave shadow

which lacks P waves, zone.

Transitivity Token Pro: verbal Value

Mood Subject Fin Pre Comp

Mood Residue Theme Theme (marked) Rheme

102. The P-wave shadow zone can be explained by the refraction of P waves when they encounter the core boundary deep within Earth’s interior.

The P-wave | canbe | explained | by the refraction of P waves when they

shadow zone encounter the core boundary deep within Earth’s interior.

Transitivity | Phenomenon Pro: verbal Circumstance Subject Fin Pre Adjunct

Mood Mood Residue

217

Theme Theme

(unmarked) Rheme

103. Because the paths of P waves can be accurately calculated, 104. the size and shape of the core can be determined also.

Because |_ the can be | accurately | calculated, | the | can | determined also paths size | be

of P and waves shape

of the

core

Tran Goal. Pro: Cir. Pro: Goal. Pro: material 1 material material 2

Sub. | Fin Adj. Pre | SUD. | Fin Pre1 2

Mood Mood. 1, Mood. 1 Mood. 2 Residue. 2

Theme Theme (marked) Rheme

105. In figure 17.8, notice 106. that Earth’s core deflects the P waves ,

In figure | notice | that | Earth’s deflects the P waves ,

17.8, core

Transitivity Cir. Pro: Actor Pro: Goal mental material . Non- . :

Adj. . Subject | Fin | Pre Complement

fin Pre

Mood Residue1 , Mood. 1 Mood. 2 Residue. 2

Theme

Theme (marked) Rheme

107. and in effect, “casts a shadow” where their energy does not reach the surface.

and in effect, “casts a where their energy does not shadow” reach the surface.

Transitivity Cir.1 Pro: material Goal Cir. 2

Adj. 1 Fin Pre Comp Adj. 2

Mood Mood Residue

Theme

Theme (marked) Rheme

108. In other words, P waves are missing within the shadow zone 109. because they have been bent (refracted) by the core.

In other P waves are | missing | within | because | they | have | bent | by the

words, the been core.

shadow

zone

: . : Pro: :

Tran Actor. 1 Pro: material | Cir. 1 Cir.2 | Goal : Cir. 3 material

Sub. 1 Fin Pre Adj. 1 Adj. 2 Sub. Fin | Pre | Adj.3

Mood Mood Residue Mood

Theme Theme Rheme

218

(marked)

110. The chapter on earthquakes explains 111. that while P waves can travel through solids and fluids,

The chapter explains | that | while | P waves | can travel through solids on and fluids, earthquakes

Pro: Cir. | Actor. R .

Tran Sayer verbal 1 1 Pro: material Cir. 2

Sub. 1 Fin | Pre Adj. Sub. 2 | Fin Pre Adj. 2

Mood ‘ 1 l ' Mood. 1 Residue.1 Mood. 2 Residue. 2

Theme

Theme (unmarked) Rheme

112. S waves can travel only through solids.

S waves can travel only through solids.

Transitivity Actor Pro: material Cir.

Sub Fin Pre Adj.

Mood Mood Residue

Theme

Theme (unmarked) Rheme

113. As figure 17.9 shows, 114. an S-wave shadow zone also exists and is larger than the P-wave shadow zone.

As | figur show, anS— | also exists and is larger than the

e wave P-wave shadow 17.9 shadow zone.

zone

Pro:

Tran Sayer | Pro: verbal | Existent | Cir. | Pro: existential relat Attribute ional

Sub. | Fi . | ow r|?Pre Sub.2 Adj. | Fin Pre . |r Comp. 2

1 n in

Mood e

Mood.1 | Res. 1 Mood. 2 Res. 2 Residue. 2

Theme Theme (marked) Rheme

115. Direct S waves are not recorded in the entire region more than 103° away from the epicenter.

Direct Š are not recorded in the entire region

waves more than 103° away from the epicenter.

Transitivity Goal Pro: material Circumstance Mood Subject a Fin Pre Resid Adjunct

Theme (unmarke d) Rheme

116. The S-wave shadow zone seems to indicate 117. that S waves do not travel through the core at all.

The S-wave shadow zone

seem

Sto

that indicate

S waves do not travel through the core

219

at all.

Tran Sayer Pro: verbal Actor Pro: material Cir.

Sub. 1 Fin Pre Sub. 2 Fin Pre Adjunct

Mood Mood Mood

Residue Theme

Theme (unmarked) Rheme

118. If this is true, 119. it implies

If| _ this is true, it implies

Tran Carrier Pro: Attribute | Sensor Pro: menrelational

Sub. 1 | Fin | Pre Comp Sub. 2 Fin Pre

Mood Mood . Mood Residue

Theme Theme (marked) Rheme

120. that the core of Earth is a liquid, or at least acts like a liquid.

the core of is a liquid, or at acts like a liquid

Earth least

Transitivity Carrier Pro: Attribute Cir. Pro: Cir. 2relational 1 material

Subject Fin | Pre | Complement Au Fin | Pre Adj. 2

Mood MoodMood Residue Theme

Theme (unmarked) Rheme

121. The way in which P waves are refracted within Earth’s core (as shown by careful analysis of seismograms) suggests

The way in which P waves are refracted

within Earth’s core(as shown by careful analysis

suggest

of seismograms)

Transitivity Sayer Pro: verbal

Subject Fin Pre

Mood Mood Residue

Theme Theme (marked) Rheme

122. that the core has two parts, a liquid outer core and a solid inner core (figure 17.7).

that the core has two parts, a liquid outer core and a solid inner core.

Transitivity Carrier Pro: Attributerelational

Subject Fin | Pre Complement

Mood Mood Residue

Theme Theme (unmarked) Rheme

Composition of the Core

220

123. When evidence from astronomy and seismic-wave studies is combined with what we know about the properties of materials,

When evidence from is combined with what we know astronomy and about the properties seismic-wave studies of materials,

Transitivity | Cir. Carrier Pro: relational Attribute Adj. Subject Fin Pre Complement Mood Mood :

Residue Theme Theme (unmarked) Rheme

124. it appears 125. that Earth’s core is made of metal—not silicate rock—

it appears that is made of metal-not Earth’s silicate rock

core

Tran Token Pro: Carrier Pro: relational Attributerelational

Mood Sub.1 | Fin Pre Sub. 2 Fin Pre Complement

Mood. 1 Res. 1 Mood. 2 Residue. 2 Theme

Theme | (unmark Rheme ed)

126. and that this metal is probably iron (along with a minor amount of oxygen, silicon, sulfur, or nickel).

and that this metal is probably iron.

Tran Carrier Pro: Cir. Attributerelational

Subject Fin | Pre Adj. Complement

Mood Mood Residue

Theme Theme (unmarked) Rheme

127. How did geologists arrive at this conclusion?

How did Geologists arrive at this conclusion?

Transitivity Cir. Pro: Actor Pro: Circumstance mat material Adj. Fin Subject Pre Adjunct

Mood Mood Residue

Theme

Theme (unmarked) Rheme

128. The overall density of the earth is 5.5gm/cm?, based on calculations from Newton’s law of gravitational attraction.

The overall 1S 5.5gm/cm’, based on calculations from density of earth Newton’s law of gravitation attraction.

Transitivity Carrier Pro: relational Attribute

Mood Subject Fin Pre Complement

221

Mood Residue

Theme Theme Rhmee(unmarked)

129. The crustal rocks are relatively low density, from 2.7 gm/cm? for granite to 3.0 gm/cm for basalt.

The crust are relatively low | from 2.7 gm/cm for granite to

rocks density, 3.0 gm/cm? for basalt.

Transitivity Carrier Pro: relational Attribute Circumstance Mood Subject Fin Pre__| Complement Adjunct

Mood Residue Theme

Theme (unmarked) Rheme

130. The ultramafic rock thought to make up the mantle probably has a density of 3.3 gm/cm? in the upper mantle,

The ultramafic rock | probably has a density of in the upper thought to make up 3.3 gm/cm3 mantle,

the mantle

Transitivity Carrier Cir. 1 Pro: Attribute Cir. 2relational

Mood Subject Adj1 | Fin | Pre | Complement Adj. 2 Mood Residue

Theme Theme (marked) Rheme

131. although rock pressure should raise this value to about 5.5 gm/cm? at the base of

the mantle (figure 17.7).

although rock should | raise this value to about 5.5 gm/cm? at pressure the base of the mantle

Transitivity Actor Pro: material Goal Circumstance

Subject Fin Pre | Complement Adjunct

Mood Mood Residue

Theme Theme (unmarked) Rheme

132. If the crust and the mantle, which have approximately 85% of Earth’s volume, are at or below the average density of Earth,

If the crust and the mantle, which are at or below the

have approximately 85% of Earth's average density of

volume, Earth,

eyes : Pro: :

Transitivity Existent : : Circumstance

existential

Subject Fin | Pre Adjunct

Mood Mood Residue

Theme Theme (marked) Rheme

133. then the core must be very heavy to bring the average up to 5.5 gm/cm’.

then the core must be very heavy to bring

the average up to 5.5 gm/cm?.

Transitivity Carrier Pro: relational Attribute

222

Subject Fin Pre Complement

Mood Mood Residue

Theme Theme (unmarked) Rheme

134. Calculations show 135. that the core has to have a density of about 10 gm/cm?

at the core-mantle boundary, increasing to 12 or 13 gm/cm at the center of Earth

(figure 17.7).

Calculations show that | the core | has | have | a density | at the core-mantle

to of about boundary, 10 increasing

gm/cm3 to 12 or 13 gm/cm` at the center of Earth

Tran Sayer Pro: Carrier Pro: Attribute Cir. verbal relational

Sub. 1 Fin | Pre Sub. 2 | Fin | Pre | Comp. Adj.

Mood Mood. 1 Residue. Mood. 2 Residue. 2

Theme

Theme (unamarked) Rheme

136. This great density would be enough to give Earth an average density of 5.5 gm/cm?.

This great would be enough to give Earth

density an average density of 5.5 gm/cmẺ.

Transitivity Carrier Pro: relational Attribute

Subject Fin Pre Complement

Mood Mood Residue

Theme

Theme (unmarked) Rheme

6.2.5. ANALYSIS OF BODY PART 5

The early case for continental drift

I. Tectonics is the study of the origin and arrangement of the broad structural

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