The Pila Spi formation composed of seven lithotypes; carbonates (dolomite and
dolomitic limestone), marl, shale/claystone, red argillaceous mudstone, sandstone,
carbonate breccias and debris flow, which are arranged in repeated cycles of mixed
siliciclastic-calciturbidites in a range of gravity-flow regime in the Koi Sanjaq area.
Sedimentologic and facies evidences suggest developed marine environment for the
Pila Spi Formation. Facies analysis and associated sedimentary structures including
graded beddings decide turbidity and gravity flow regime origin of the rocks.
Marine environment is supported by the identifying glauconite and fossils types,
which is reported here for the first time rather than lagoon environment.
The Pila Spi sequences are grouped into four facies associations confirming
developed marine depositional systems, these are (from bottom to top) channeledslumped
fine and mega carbonate breccias, calciturbidites, faulted and slump
carbonate mega-breccias, slump/slide carbonate mega-breccias facies associations
respectively.
Petrographic analysis of carbonate units of the Pila Spi rocks in Koi Sanjaq area
indicated that they are composed of skeletal grains with subordinate non-skeletal
grains of tuffaceous fragments, chert, chalcedony, volcanic ash, metamorphic and
detrital iron oxides grains, with noticeable grains of glauconite. Varieties of marine
fossils are identified includes planktonic bivalves and benthic forams of cool water,
which support the deeper marine environment.
Microfacies analysis reveals (15) types, these are; green algal boundstone, algal
wackestone dolomudstone, algal dolostone/mudstone, framestone-mudstone, small
benthic foraminiferal wackestone, algal packstone-mudstone, foraminiferal
packstone-mudstone, algal dolostone, fossiliferous grainstone, foraminiferal
packstone, stromatolite framestone, algal boundstone, calci-microbial grainstonepackstone,
and large benthic Foraminiferal bioclasts floatstone. These microfacies
types are grouped in four facies associations representing the depositional
environments of the formation, these are; outer shelf, reef, forereef, reef, backreef.
Due to the importance of solutions of partial differential equations, linear, nonlinear, homogeneous, and non-homogeneous, in important life applications, including engineering applications, physics and astronomy, medical sciences, and life technology, and their importance in solutions to heat transfer equations, wave, Laplace equation, telegraph, etc. In this paper, a new double integral transform has been proposed.
In this work, we have introduced a new double transform ( Double Complex EE Transform ). In addition, we presented the convolution theorem and proved the properties of the proposed transform, which has an effective and useful role in dealing with the solution of two-dimensional partial differential equations. Moreover
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, followed by its application to solving the forward and inverse problems. This model is then extended to the general case and the advantages and di sadvantages of this approach are descri bed along with an analysis of the sensi tivity of
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This work pr
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The current study aimed to assess the severity of anaemia, evaluate the current treatment guideline of anaemia, and to determine the association between the level of anaemia and its treatment on quality of life of breast cancer patients in Malaysia. This prospective study conducted among breast cancer patients in multicancer centers in Malaysia including three follow ups after receiving their chemotherapy. Clinical data were collected from their medical records and at each follow up, they asked
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