Upper Cretaceous Oceanic Red Beds (CORBs) are pelagic sediment
deposits that deposited in the Upper Cretaceous basin, with widespread in
part of the world as well as in Iraq. This research investigates the deposition
of cyclic marl and marly limestone CORBs of six selected sections at the
active southern margin of the Tethys during the Late Campanian -
Maastrichtian with petrography, microfacies, and depositional environment.
As this study was not a consideration in the past, so decided to visit and
identify all exposure areas of the Upper Cretaceous period rocks are visited.
This study involved two fields touring reconnaissance extended from
Darbandikhan city in the east south to Shiranish Village in the west north.
Six lithological sections covering the studied area, four sections represent
Cretaceous Oceanic Red Beds (CORBs) and two sections without (CORBs)
for the purpose of comparison between them. The sections are described in
detail and 250 samples were collected from all studied sections.
For the petrography and microfacies analysis 149 thin sections were
studied. The microfacies analysis showing two major successions with Red
Bed and Non-Red Bed marl and marly limestone, occasionally interbedded
with thinly beds of shale, sandstone and siltstone. These comprised of five
microfacies are Oligostegina Marly Limestone, Globotruncana Marly
Limestone, Marlstone with Microfossils, Red Marlstone, and Red to
Variegated Calcareous Sandstone with Radiolarian (Debrise Flow) Making
20 thin sections from Gendilly section(GS) (the typical section of this study)
for microscopic study of minute fossils (nannofossils) examination, for this
study proved that the Cretaceous Oceanic Red Beds (CORBs) dating is
Mastrichtian age. The Microfossils and nannofossils tests proved the
presence of Danian Age in studied area.
This study has proved that the carbonate content in red limestone beds
ranged between 53.5-100.0 %, while this percentage ranged in red marly
rocks between 20.5-50.0 %, But in the rocks that do not contain red beds,
Carbonate content in limestone rocks ranged between 52.0-100.0 %, and in
marl rocks this ratio ranged between 27.5-49.5 %.
ان من اهم القضايا التي تثيرها المعرفة البشرية في تجلياتها، وتعبيراتها المفاهيمية، تكمن في مدى تأصلها وانتمائها الى البنى والتشكيلات الموضوعية (في مستوياتها التاريخية) التي تسعى لتفسيرها وادراكها ومضاهاتها. فالينبوع الذي يغرف منه الفكر مادته هو الكيان الاجتماعي المتموضع خارج الوعي والايدولوجيا.
ان قدرة الوعي على ادراك الواقع الموضوعي بخصائصه العامة يشكل الشرط الضروري لاكتساب الوعي ل
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1) Fine hiogenic dolomite facies.
2) Sandy rich dolomite facies.
3) Dolomite diagenetic facies.
4) Recrystal1ized wackestone in microfacies.
5) Mudsione facies.
Microfacics reflect shallow marine water with open Circulation in the lower part of the formation and the environment of the upper is enclosed between upper tide and tide. The most important diagenesis was recrystallization and spary calcite deposit inside fossils chambers and pores.
This work was included external morphological study of male Black veined white butterfly Aporiacrataegi L. 1758. The study involved morphological characters of many body regions, in addition the male genitalia. This morphological characters study supported by illustrations, it should be noted the work specimens were collected from northern Iraq.