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PROVENANCE OF KARAKUM DESERT SAND (TURKMENISTAN):

LITHIC-RICH OROGENIC SIGNATURE OF CENTRAL ASIAN DUNE FIELDS

EDUARDO GARZANTI, MOHAMMAD R. GHASSEMI

, MARA LIMONTA

& ALBERTO RESENTINI

Rivista Italiana di Paleontologia e Stratigrafia

(Research in Paleontology and Stratigraphy)

vol. 125(1): 77-89.

March 2019

(2)

Garzanti E., Ghassemi M.R., Limonta M. & Resentini A.

ii

Riv er Site Sam ple Operator GSZ Q KF P Lvf Lvm Lcc Lcd Lp Lh Lms Lmv Lmf Lmb Lu mi ca HM Q F L Lm Lv Ls Qp/Q P/F Mi c/F MI* MI Pan j Kis ht i P oy en S47 48 A.Res en tini 110 40 5 12 0,3 1 11 4 3 ----7 1 4 0,5 0,3 3 8 100,0 46 19 36 100,0 26 5 69 100,0 0,1 2 0,7 0 0,0 5 224 165 Yak hs u Dar a-Khu rda k S47 49 A.Res en tini 180 11 0,3 2 ----52 10 1 ----14 1 6 0,3 0,3 2 1 100,0 11 3 86 100,0 16 1 83 100,0 0,2 9 0,8 9 0,0 0 214 205 Khi ng ou O bi khi ng ho b S47 51 A.Res en tini 120 28 1 10 ----1 19 4 5 ----14 1 2 3,6 0,6 3 9 100,0 32 12 56 100,0 26 2 72 100,0 0,4 4 0,9 1 0,0 0 215 171 Vak hs h Chu m do n S47 50 A.Res en tini 170 32 2 9 1 1 10 4 6 ----12 5 3 5,3 ----1 8 100,0 36 12 52 100,0 36 8 55 100,0 0,3 0 0,8 4 0,0 6 216 168 Har i Rud G us h S ar go us i S34 63 G .Rad ef f 210 38 9 13 4 5 8 0,3 1 ----9 5 4 ----0,9 2 1 100,0 40 22 38 100,0 30 32 38 100,0 0,1 5 0,5 8 0,0 2 199 131 eo lian d un e As hk -A ba d S53 35 A.Res en tini 100 49 3 17 1 1 12 1 1 0,3 5 3 1 1,7 ----0,3 6 100,0 52 21 27 100,0 26 10 64 100,0 0,2 1 0,8 5 0,0 6 200 175 eo lian d un e Or fa S41 9 G .Rad ef f 360 29 9 6 2 2 37 0,4 8 1 3 3 1 0,2 ----100,0 29 15 56 100,0 7 8 85 100,0 0,0 7 0,3 9 0,0 2 187 62 eo lian d un e Tu ar S41 8 G .Rad ef f 350 48 12 9 4 3 4 ----4 2 3 9 2 ----100,0 48 21 31 100,0 26 38 37 100,0 0,1 8 0,4 4 0,0 6 149 75

Tab

A2 -

Sand

petrog

raph

y. GSZ = g

rain

size

. Q = quar

tz (Qp = polycr

ystalline);

F

= feldspars (KF

= K-feldspar;

P

= plagioclase;

Mic = cross-hatc

hed microcline);

L =

aphanitic lithic

grains

(Lv

= v

ol

-canic

and

sub

volcanic;

Lvf

=

felsic

volcanic

and

sub

volcanic;

Lvm

=

mafic

and

inter

mediate

volcanic

and

sub

volcanic;

Ls

=

sedimentar

y;

Lcc

=

lime

stone;

Lcd

=

dolostone;

Lp

=

shale/siltstone;

Lh

=

cher

t;

Lm

=

metamor

phic;

Lms

=

lo

w-rank

metasedimentar

y;

Lmv

=

lo

w-rank

meta

volcanic;

Lmf

=

high-rank

metapelite/metapsammite/m

etafelsite;

Lmb

=

high-rank

metabasite;

Lu=

ultramafic).

HM=

hea

vy

minerals

. T

he

metamor

phic

indices

MI

and

MI*

express

the

averag

e

metamor

phic

rank

of

roc

k

fragments

in

eac

h

sample

. MI

varies

from

0

(detritus

shed

by

ex

clusi

vely

sedimentar

y

and

volcanic

co

ver

roc

ks

) to

500

(v

er

y-high-rank

detritus

shed

by

ex

clusi

vely

high-g

rade

basement

roc

ks).

MI*

considers

only

metamor

phic

roc

k

fragments

, and

thus

varies

from

100

(v

er

y-lo

w-rank detritus shed b

y ex

clusi

vely v

er

y lo

w-g

rade metamor

phic roc

ks) to 500 (Garzanti & V

ezzoli 2003).

Samp

le

Riv

er /

Des

ert

Site

Fa

cie

s

Coun

try

Coll

ec

te

d by

Year

La

titu

de

Lo

ng

itu

de

S4748

Panj

Kis

ht

i P

oy

en

sandy

riv

er

bar

Tajik

is

ta

n

Paol

o B

al

lat

o

2013

37°

56

'45"

N

70°

11

'30"

E

S4749

Yak

hs

u

D

ar

a-Khur

dak

sandy

riv

er

bar

Tajik

is

ta

n

Paol

o B

al

lat

o

2013

38°

26

'30"

N

70°

02

'30"

E

S4751

Khi

ng

ou

Ob

ik

hing

ob

sandy

riv

er

bar

Tajik

is

ta

n

Paol

o B

al

lat

o

2013

38°

52

'00"

N

70°

02

'00"

E

S4750

Vak

hs

h

C

hum

don

sandy

riv

er

bar

Tajik

is

ta

n

Paol

o B

al

lat

o

2013

38°

52

'30"

N

70°

03

'00"

E

S4632

Syr

D

arya

Bur

am

at

ut

u

sil

ty r

iv

er lev

ee

U

zbek

istan

P.K

ru

gm

ier

/G.

M

.Zan

de

righ

i

2009

40°

53

'00"

N

71°

26

'30"

E

S3463

Ha

ri

G

us

h S

ar

gous

i

sandy

riv

er

bar

Ira

n

Eduar

do G

arz

ant

i

2005

36°

21

'59"

N

61°

09

'01"

E

S5335

Kar

ak

um

As

hk

-A

bad

eol

ian dune

Tu

rkm

eni

stan

Saei

d S

abour

i

2017

38°

04

'00"

N

58°

21

'30"

E

S419

Kar

ak

um

O

rfa

eol

ian dune

Tu

rkm

eni

stan

Eduar

do G

arz

ant

i

1997

40°

16

'00"

N

54°

12

'00"

E

S418

Kar

ak

um

Tua

r

eol

ian dune

Tu

rkm

eni

stan

Eduar

do G

arz

ant

i

1997

40°

50

'30"

N

55°

11

'00"

E

Tab

. A1

- Infor

mation

on

moder

n

sediment

samples

. Location

of

the

studied

fluvial

and

eolian

sediments

is

indicated

also

in

the

Google

Ear

thTM file T

urkmen.kmz.

(3)

Provenance of Karakum desert sand (Turkmenistan)

iii

Ri

ve

r

Site

Sam ple O per at or clas s ana lyse d %fine r %cla ss %coa rser met hod tHM c ount ed tota l g rai ns HM %wei ght tHM % weigh t zirco n tour mal ine rut ile tita nite apat ite epido te gar net chl orito id sta urol ite anda lus ite kyan ite sillim anit e amp hibol e clino pyrox ene hype rsth ene spi nel axini te barite Tot al Sy r Dar ya l ev ee Bur am at ut u S46 32 M .L im on ta 15-500 60% 36% 4% Poi nt 207 332 1,5 1,5 5 2 ----4 9 26 11 ----1 ----0,5 41 1 ----100,0 Pa nj Kis ht i Po ye n S47 48 M .L im on ta 32-500 6% 94% ----Poi nt 211 325 6,3 5,9 1 1 ----0,5 3 43 6 ----2 0,5 0,5 2 36 5 ----100,0 Yak hs u Dar a-Khu rda k S47 49 M .L im on ta 32-500 8% 76% 16% Poi nt 211 548 1,2 1,2 1 6 2 ----5 44 21 0,5 0,5 ----0,5 20 ----100,0 Khi ng ou O bi khi ng ho b S47 51 M .L im on ta 32-500 8% 92% 0,02% Poi nt 206 290 6,2 6,2 1 1 ----1 69 6 ----3 ----0,5 0,5 16 1 ----100,0 Vak hs h Chu m do n S47 50 M .L im on ta 32-500 4% 96% 0,04% Poi nt 202 238 9,2 9,1 ----0,5 ----0,5 71 8 ----20 ----100,0 Har i Rud G us h S ar go us i S34 63 M .L im on ta 32-500 6% 94% ----Poi nt 235 421 2,9 2,3 5 3 2 1 4 28 9 ----1 0,4 ----1 26 17 1 1 ----1,3 100,0 eol ia n d une As hk -A ba d S53 35 M .L im on ta 32-500 ----100% ----Poi nt 207 243 4,7 4,6 3 0,5 0,5 0,5 2 54 10 ----1 ----25 3 ----0,5 ----100,0 eol ia n d une O rfa S4 19 M .L im on ta 32-500 2% 98% ----Poi nt 211 302 2,3 1,9 5 1 0,5 0,5 1 43 11 ----0,5 1 31 4 1 ----100,0 eol ia n d une Tu ar S4 18 M .L im on ta bu lk ----100% ----Fle et 207 1196 1,6 0,5 13 2 1 ----3 44 18 ----0,5 ----14 5 ----100,0

Ri

ve

r

Site

Sam ple O per at or HCI MMI ZTR % tr anspa ren t HM % o paqu e HM % F e oxide s % T i oxid es % tu rbi d HM % roc k fr agm ents % s oils & alte rite s % c hlor ite % b iotit e % c arbo nate s & li ght m ine ral s Tot al Sy r Dar ya l ev ee Bur am at ut u S46 32 M .L im on ta 17 n.d. 7 62% 1% 0% 0% 0% 1% 25% 2% 6% 1% 0% 100% Pa nj Kis ht i Po ye n S47 48 M .L im on ta 21 67 2 65% 2% 3% 0% 0% 2% 16% 3% 7% 1% 0% 100% Yak hs u Dar a-Khu rda k S47 49 M .L im on ta 7 n.d. 9 39% 1% 0% 0% 0% 5% 34% 11% 7% 2% 0% 100% Khi ng ou O bi khi ng ho b S47 51 M .L im on ta 16 44 2 71% 0% 0% 0% 0% 2% 15% 2% 7% 1% 0% 100% Vak hs h Chu m do n S47 50 M .L im on ta 19 n.d. 0 85% 0% 0% 0% 0% 2% 11% 0% 1% 0% 0% 100% Har i Rud G us h S ar go us i S34 63 M .L im on ta 19 67 10 56% 6% 6% 3% 0% 1% 22% 3% 2% 1% 0% 100% eol ia n d une As hk -A ba d S53 35 M .L im on ta 26 n.d. 4 85% 0% 1% 0% 0% 0% 12% 0% 2% 0% 0% 100% eol ia n d une O rfa S4 19 M .L im on ta 20 n.d. 6 70% 4% 10% 1% 0% 1% 13% 0% 1% 0% 0% 100% eol ia n d une Tu ar S4 18 M .L im on ta 19 n.d. 15 17% 8% 28% 3% 0% 0% 42% 0% 0% 2% 0% 100%

Table

A3

- Hea

vy

minerals

. HM=

hea

vy

minerals;

tHM=

transparent

hea

vy

minerals;

n.d.

=

not

deter

mined.

The

ZTR

index

(sum

of

zircon,

tour

maline

and

rutile

ov

er

total

transparent

hea

vy

minerals)

ev

aluates

the

“c

hemical

durability”

of

the

detrital

assemblag

e

(Huber

t 1962;

Garzanti

2017).

The

HCI

(Hor

nblende

Colour

Index)

and

MMI

(Met

asedimentar

y

Minerals

Index)

var

y

from

0

in

detritus

from

greensc

hist-facies

to

lo

w

er

most

amphibolite-facies

roc

ks

yielding

ex

clusi

vely

blue/g

reen

amphibole

and

chloritoid,

to

100

in

detritus

from

gran

ulite-facies

roc

ks

yielding

ex

clusi

vely

bro

wn hor

nblende and sillimanite

, and are used to estimate the a

verag

e metamor

phic g

rade of

metaigneous and metasedimentar

y source roc

ks

, respecti

(4)

Figura

Tab  A2 -  Sand  petrog raph y. GSZ = g rain  size . Q = quar tz (Qp = polycr ystalline);  F  = feldspars (KF  = K-feldspar;  P  = plagioclase;  Mic = cross-hatc hed microcline);  L =  aphanitic lithic  grains  (Lv  = v ol -canic and subvolcanic; Lvf = fel
Syr Darya leveeBuramatutuS4632M.Limonta17n.d.762%1%0%0%0%1%25%2%6%1%0%100% PanjKishti PoyenS4748M.Limonta2167265%2%3%0%0%2%16%3%7%1%0%100% YakhsuDara-KhurdakS4749M.Limonta7n.d.939%1%0%0%0%5%34%11%7%2%0%100% KhingouObikhinghobS4751M.Limonta1644271%0%0%0%0%2

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