the red sea rifting: tectonic history and stratigraphic successions

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- 391 Middle East Geology -Geol 501-142 The Red Sea rifting: Tectonic history and Stratigraphic successions By: Abdullah Alqubalee [email protected] KFUPM Earth Science Department May 05, 2015

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Page 1: The Red Sea rifting: Tectonic history and Stratigraphic successions

-391 Middle East Geology -Geol 501-142

The Red Sea rifting: Tectonic history and Stratigraphic successions

By:

Abdullah [email protected]

KFUPMEarth Science Department

May 05, 2015

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Outline• Introduction.• Tectonic History of the Red Sea.• The Red Sea stratigraphy and Petroleum System.• Geology and Stratigraphy of Midyan, SA.• Conclusion.

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Introduction

(Bosworth et al., 2005)

AFFZ = Alula-Fartaq fracture zone;BM = Bab al Mandeb;D = Danakil horst;DA = Dahlak archipelago; ET = Ethiopian trap series;G = Cape Gwardafuy;GOA = Gulf of Aqaba;GOS = Gulf of Suez; MAP = Makran accretionary prism;MER = main Ethiopian rift; MS = Mesozoic Marib-Shabwa (Sab’atayn) Basin;SI = Socotra Island; SOC = Semail oceanic crust; SR = Sheba Ridge;S = Shukra al Sheik discontinuity;RS = Ras Sharbithat; YT = Yemen trap series;ZI = Zabargad Island

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Introduction

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Objectives• To demonstrate the tectonic history and the Stratigraphic

succession of the Red Sea.

• To demonstrate the Cenozoic Stratigraphy of Midyan Region, Saudi Arabia.

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Tectonic History of the Red Sea

(Bosworth et al., 2005)

Early

Olig

ocen

eO

ligoc

ene–

Mio

cene

tran

sitio

n

Mid

dle

Mio

cene

Late

Olig

ocen

e

Oceanic spreading started on eastern Sheba Ridge by 19 Ma

Palin

spas

tic re

stor

ation

of t

he R

ed S

ea–G

ulf o

f Ade

n rift

syst

em

Page 7: The Red Sea rifting: Tectonic history and Stratigraphic successions

-397 Middle East Geology -Geol 501-142(Bosworth et al., 2005)

Early

Lat

e M

ioce

nePr

esen

t-day

situ

ation

Prop

osed

futu

re g

eom

etry

Mio

cene

–Plio

cene

tran

sitio

n

Palin

spas

tic re

stor

ation

of t

he R

ed S

ea–G

ulf o

f Ade

n rift

syst

em

Tectonic History of the Red Sea

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Summary of Tectonic History of the Red SeaEarly Oligocene Afar plume initiation & older Harrats formation.

Late Oligocene Gulf of Aden initiation & Eritrean Red Sea continental rift.

Oligocene–Miocene transition

Rapid spread of extension throughout Red Sea.

Middle Miocene

Onset of Aqaba–Levant transform boundary and by-passing of Gulf of Suez basin

Oceanic spreading started on eastern Sheba Ridge by 19 Ma.

Early Late Miocene Rift–drift transition in central Gulf of Aden.

Miocene–Pliocene transition

Rift–drift transition in south-central Red Sea, jump of spreading west of 45E in Gulf of Aden (perhaps 3 Ma), and acceleration of Aqaba–

Levant movement.Tect

onic

Hist

ory

of

the

Red

Sea

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Arabian Plate Reconstruction, Early Cenozoic to latest Eocene.

(Sharland et al,. 2001)

Tect

onic

Hist

ory

of

the

Red

Sea

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Arabian Plate, latest Eocene to Present.

(Sharland et al,. 2001)

Tect

onic

Hist

ory

of

the

Red

Sea

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Stratigraphic correlation a long the length of the red sea

(Bosworth et al., 2005)

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Chronostratigraphic section for AP11.

(Sharland et al,. 2001)

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Stratigraphy of the Red Sea, Saudi Arabia

Source : (Hughes et al,. 2005)

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Stratigraphy of the Red Sea, Saudi Arabia

Source : (Hughes et al,. 2005)

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Stratigraphy of the Red Sea, Saudi Arabia

Source : (Hughes et al,. 2005)

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Cenozoic Stratigraphy of Midyan, Saudi Arabia

(Bosworth et al., 2005)

(Hughes et al., 1999)

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Satellite image Midyan, Saudi Arabia

(Hughes et al., 1999)

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Geologic map of Midyan, Saudi Arabia

(Hughes et al., 1999)

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Stratigraphy- Midyan, Saudi Arabia

(Hughes et al., 1999)

Fluvio-lacustrine

Restricted marine

Intertidal-shallow marine

Bathyal

Turbidites

Bathyal

Hypersaline submarine

Deep Hypersaline marine

Shallow to marginal-marine

Fluvial & delta-plain

Paleoevnironment

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Conclusion• The Gulf of Aden and the Red Sea rifting were initiated in Late

Oligocene, ~25 Ma.• The Triple Junction lying above the Afar Hot Spot is RRR type. • AP11 lasted 34 Ma is defined as the package of sediments lying

between the unconformity marking both the onset of Red Sea rifting and the first continent-continent collision, Zagros collision.

• Several tectonic phases are defined that fall into the categories of pre-rift, syn-rift, and post-rift.

• The Red Sea current reservoirs are : Jabal Kibrit, Umm luj mbr, Wadi Waqb mbr, and Burqan formation.

• AlWajh formation is considered as a prospective reservoir.• The Midyan region provides a unique view of the Red Sea subsurface

stratigraphy of Saudi Arabia.

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References• Bosworth, W., Huchon, P., & McClay, K. (2005). The red sea and gulf of Aden basins.

Journal of African Earth Sciences, 43(1), 334-378.

• Hughes, G. W., Perincek, D., Grainger, D. J., Abu-Bshait, A. J., & Jarad, A. R. M. (1999). Lithostratigraphy and depositional history of part of the Midyan region, northwestern Saudi Arabia. GeoArabia, 4(4), 500-542.

• Hughes, G. W. A., & Johnson, R. S. (2005). Lithostratigraphy of the Red Sea region. GeoArabia, 10(3), 49-126.

• Sharland, P. R., Archer, R., Casey, D. M., Davies, R. B., Hall, S. H., Heward, A. P., ... & Simmons, M. D. (2001). Arabian plate sequence stratigraphy. GeoArabia.