The Crystalline Basement rocks is located in

Age of Crystalline Basement rocks is

Crocker and Trusmadi Formation are the _______ unit in Sabah.

Crocker & Trusmadi Fm. lithologies consist of

The Crocker & Trusmadi Fm. are ________.

Crocker and Trusmadi Formation are interpreted as ___________ formed during __________of proto-South China Sea beneath Sabah.

Sabah Orogeny created the _________ Top-Crocker unconformity.

Sabah Orogeny was followed by the deposition of __________ formations, preserved in ______ Sabah (Hutchison, 2005; Hall, 2013).

Since there is no _______ which discuss the overall geology of whole Sabah, the geology is thus describe according to area.

Western & North Sabah consist of ________ and subordinate ________ rocks

The age of rocks in Western & North Sabah is

Rocks in Western & North Sabah has undergone several episodes of _________.

The deformation of Western & North Sabah probably occured during

The deformation of Western & North Sabah thought to have controlled the development of an elongate basin trending approximately ____ and ____.

The elongate basin in Western & North Sabah later became the site for deposition of ___________ sediments.

The elongate basin in Western & North Sabah later became the site for deposition of sediments from which formations?.

The lithology of the sedimentary rocks in Western & North Sabah

The lithology of the metamorphic rocks in Western & North Sabah

The lithology of the igneous rocks in Western & North Sabah

Which is the Oldest dated sedimentary rocks in Western & North Sabah?

In Western & North Sabah, the Thinly bedded cherts is closely associated with _______ type of _______ igneous rocks.

In Western & North Sabah, the basaltic igneous rocks is closely associated with

The association of rock types in Western & North Sabah, which resembles an _________ series, is interpreted to represent an _______ crust of _________ age, and forms the basement rock of this region.

The ___________ age sedimentary rock in Western & North Sabah lies ________ on the basement rock.

The sedimentary rocks that lies on the basemen rocks in Wester& North Sabah are represented by which formations?

The Crocker and Trusmadi Formations occur mostly in which part of Sabah?

Crocker and Trusmadi Formations are mostly ______ water ______ sediments.

The sediments of Crocker and Trusmadi Formations are characterised by rythmic alternation of ______________ beds

Kudat Formatioc occurs in _____ Sabah.

Kudat Formation is ___________ sediments.

characterised by ___________ and ______ with lenses of Eocene-Early Miocene biohermal limestones

The age of biohermal limestones in Kudat Formatio.

The lithology of Bongaya Formation

Bongaya Formation lie _________ on the basement rock, Crocker and Kudat Formations in Northern Sabah.

The deposits of Bongaya Formation overlain ________ by shallow water sediments of ________ Formation.

The age of Timohing Formation that overlies Bongaya Formation is

The Timohing Formation overlying the Bongaya Formation can be found at _____________.

The intrusive and extrusive igneous rocks of Western and North Sabah were formed during ____________ times.

Which is the intrusive igneous rocks in Western & North Sabah?

The Interbedded sandstone and shale of Crocker Fm deposited in a ________ basin.

What is the deep water basin of interbedded sandstone and shale in Crocker Formation?

The Interbedded sandstone and shale deposition of Crocker Fm occured during which age?

Crocker Range runs ________ and is deformed by a series of high angle _________ faults dipping south or south-east.

The reverse fault that deformed Crocker Fm probably formed during

In Crocker Fm, the soft shale layers have often acted as ________ for the faults and deformation

Tongkul divided the turbidites of Crocker Formation into two units which are

The thickness of the lower sandstone unit of the Crocker F. turbidites.

The thickness of the upper shale unit of the Crocker F. turbidites.

The lower sandstone unit of the Crocker Fm turbidites is an alternation of thick _____________ beds and relatvely thin ____________ beds.

The sandstone in lower sandstone unit of Crocker Fm turbidites is

Upper shale unit of Crocker Fm turbidites occurs as a ________ of grey or red shale

Crocker turbidites are also exposed on islands offshore ___________.

Crocker turbidites extend offshore _______ Sabah below the Miocene-Quaternary _______ sediments

The relationship between the Crocker and Trusmadi formations is probably

The basement rock of Crocker Fm of Sabah is

The basement rock of Crocker Fm is probably _______ age.

The ophiolite melange that is the basement rock in Crocker Formation is __________ rocks.

The northern part of Sabah, consisting of ___________ rocks of __________ age

North Sabah has experienced three major episodes of deformation associated with _______ and ______ oriented compressions.

The earliest episode deformed and uplifted an oceanic basement which is the

The earliest episode deformed and uplifted an oceanic basement to form an elongate basin trending __________ during ___________ times.

The elongate basin formed in North Sabah became the site for the deposition of middle Eocene to Early Miocene _______ sediments

The elongate basin of Crocker Formation became the site for the deposition of Crocker and Kudat formations, sourced from continental basement towards the _______ and ______, respectively

Kudat Peninsula comprises of four formations which are

Kudat Peninsula is dominantly made up of

The Kudat Formation is a relatively _______ to ________ sea sediments

The _______, ________ and ________ Members of Kudat Formation are made up of interbedded sandstone and mudstone

The Gomantong Member referred to as the ______ Unit of Kudat Formation by Tongkul

Gomantong Memberpossibly describing this unit as the _______ member

Gomantong Member consists of interbedded medium to fine-grained ________ , predominantly sandstone layer

The sandstone bed is characterized by sedimentary structures such as _________, ________, _________, and ________.

The Sikuti Member of Kudat Fm is made up of interbedded fine-grained __________ and ________with abundance sedimentary structures.

The Sikuati Member contain abundance of sedimentary structures which are

Tajau Member comprises of thick _______bed interbeds with thin ________ layer

The Tajau Member of Kudat Formation was formed the _______ Kudat terrane

The of Tajau Member in Kudat Fm

Fossil evidence in Tajau Member of Kudat Fm

The Melange unit of Kudat Fm is found in few localities mostly in the __________ part of peninsula.

The mélange unit of Kudat Fm appears within a strip zone, bounded by major _______.

The melange unit of Kudat Fm is situated in between ________ and ________.

The melange unit of Kudat Fm is made up of an intensely deformed mixture of the ________ basement rock

The melang unit of Kduat Fm is presence in the form of -________ and ________ structures.

Blocks of rocks that were identified in the mélange unit of Kudat Fm are

The knocker found on the Kudat peninsula is a boulder of chaotic unit comprising of ______, ______ and _______.

The knocker found on the peninsula originated from the basement rock that had been _______ to the surface

The melange unit of Kudat Fm is ________ characterized by folds and refolded folds

This mélange strip found in a faulted zone of ________ fault, indicated by the _______ surface of serpentinite showing dextral sense of movement

Presence of ___________ (NN6) and other associated nannofossils in the mudstone of the mélange unit is dated _______ in age