Previous Page  199 / 352 Next Page
Information
Show Menu
Previous Page 199 / 352 Next Page
Page Background

183

and an average of 21 ppm of Pb (minimum:

2, maximum: 103; Appx. 4). Th/U ratios have

average values of 0.34 (minimum: 0.001,

maximum: 0.94; Fig. 77a).

176

Lu/

177

Hf ratios plot around 0.00141 ±

0.00128

r

2 SD; Fig. 77b).

176

Yb/

177

Hf ratios plot

around 0.0446 ± 0.0420

r

2 SD; Appx. 4).

Nd whole-rock model-age is 1.08 Ga and

H

Nd

(t)

values are:

H

Nd

(t=0)

= -3.6;

H

Nd

(t=500)

= +0.6.

7.4.4.2. Discussion

Zircon from this sample shows a high variety

of textures and chemical ratios and values. It has

not beenpossible to relate these observations with

certain age ranges. The maximum abundance

peak of 500Ma is interpreted as the age of igneous

crystallisation of the protolithic felsic magmas.

The relative abundance peak of 470 Ma zircon

is interpreted as a Pb-loss process triggered by

the

c.

390 Ma HP–HT metamorphic event or

by a

c.

470 Ma metamorphic event that altered

the previous protolithic

c.

500 Ma zircon. This

possible

c.

470 Ma event could be a temperature

input related to the arc development in which

this sample is related to. Almost all zircon grains

show structure-less bright rims which in some

cases are sinuous and transgressive. One analysis

on a bright rim gave an age of 390

r

8 Ma (A236;

Fig. 75). This age is repeatedly present in many

samples and it is interpreted as the age of HP–

HT Devonian metamorphism and could explain,

by Pb-loss process, the relative abundance of

470 Ma zircon in this sample. This felsic rock

outcrops together with a

c.

507 Ma mafic rock

(GCH-23, section 7.3.4) and both lithologies

outcrop together with field relationships

interpreted as a mingling process between them.

It is interpreted that this felsic rock intruded at

c.

500 Ma the

c.

507 Ma mafic rock and triggered

a high temperature input. Sample GCH-23 also

shows a relative abundance of ages at

c.

470 Ma

Fig. 73.

U-Pb conventional concordia diagram showing

U-Pb zircon analyses of the studied sample. Ellipses repre-

sent combined 2

σ

uncertainties of

206

Pb/

238

U and

207

Pb/

235

U

ratios.

n

, number of analyses considered (those with 90–

110% concordance)/total number of U–Pb analyses.

3E 8

GDWD SRLQW HUURU HOLSVHV DUH ı

3E 8

*&+

2UWKRJQHLVV

Q

Fig. 74.

Adaptative Kernel Density Estimation (aKDE, continuous line enclosing the blue area), Probability Density (PDP,

black dashed line) and histogram diagrams of the U–Pb analyses (calculated with DensityPlotter5.0, Vermeesch 2012).

Numbers in the vertical axis represent histogram frequency;

n

, number of analyses.

a

Partial plot representing data within

a 300–700 Ma time range (bandwidth = 5 Ma, binwidth = 5 Ma).

b

Complete plot (bandwidth = 15 Ma, binwidth = 25 Ma).

3DOHRSURWHUR]RLF

0HVR

SURWHUR]RLF

3DOHR]RLF DQG

1HRSURWHUR]RLF

$UFKHDQ

>0D@

Q

Q

D

E

7.4. ORTHOGNEISSES