Eustatic, tectonic and climatic controls on an early syn-rift mixed-energy delta, Tilje Formation (Early Jurassic, Smørbukk field, offshore mid-Norway) - From Depositional Systems to Sedimentary Successions on the Norwegian Continental Margin - page 341

Tectonic
Movement

Chronostratigraphy Lithostratigraphy

Volgian

SPEKK

III

Oxfordian

ROGN

Kimmeridgian

Intra-Melke Unconformity

Callovian

MELKE

II

Bathonian

GARN

Bajocian

NOT

Aalenian

ILE

Toarcian

TOFTE

ROR

I

Pliensbachian

TILJE

Sinemurian

ÅRE

Hettangian

Rhaetian

GREY/RED BEDS
UPPER SALT
RED BEDS

Norian

Karnian

(B)

4 ° 00 ʹ 6 ° 00 ʹ 8 ° 00 ʹ 10 ° 00 ʹ 12 ° 00 ʹ 14 ° 00 ʹ

N

67 ° 00 ʹ

66 ° 00 ʹ

Mosjøen

Halten
Terrace

NORWAY

Shallow Marine

65 ° 00 ʹ

Tide and wave
dominated marginal

Smørbukk
(Åsgard)

Marginal to alluvial
plain

Basement/bed rock

Frøya High

Area of erosion

64 ° 00 ʹ

Tilje Seaway

0 100 km

Fig. 2. (A) Summary of Triassic and Jurassic lithostratigraphy and tectonic events in the Halten Terrace area. The tectonic-
movement column shows main pulses of rifting that had an impact on the geometry of Jurassic reservoirs: (I) Early Jurassic,
(II) Middle Jurassic and (III) Late Jurassic times. (B) Lower Jurassic palaeo-geographic setting of the Halten Terrace and the
Early Jurassic seaway elements. Compiled and modified from Doré (1991), Brekke et al . (2001).