Студопедия
Случайная страница | ТОМ-1 | ТОМ-2 | ТОМ-3
АвтомобилиАстрономияБиологияГеографияДом и садДругие языкиДругоеИнформатика
ИсторияКультураЛитератураЛогикаМатематикаМедицинаМеталлургияМеханика
ОбразованиеОхрана трудаПедагогикаПолитикаПравоПсихологияРелигияРиторика
СоциологияСпортСтроительствоТехнологияТуризмФизикаФилософияФинансы
ХимияЧерчениеЭкологияЭкономикаЭлектроника

New method of investigation of bentic Foraminifera assembly across Paleocene - Eocene in north Schousf (Nehbandan), east of Iran

Читайте также:
  1. A Northland Miracle
  2. A Short Historical Outline of Typological Investigations
  3. Acceptance. Methods of acceptance
  4. AND NORTHERN IRELAND
  5. Antenna Assembly
  6. Attitude, Methodology & Technology.
  7. Auxiliary techniques of investigation

 

Bahramali A.

Geological Survey of Eastern Iran, Payamenoor University, Tehran, Iran

alibahramali@Gmail.com

In this Research I study the section that is exist in north of Schousf at southern Khorasn province. I collected totally 78 thin section at profile.

The longitude of my section is 60 18´-60 13´ Eastern and its latitude is 31 47´52˝-31 52´44˝. northern based on these analyses, from the bottom to up I have three Sequences in this section.

The layers from the 1-35th belong to CHAH CHO CHO formation and 36th-41th layers belong to the formation that called ZIBRO and the formation that pertain to 42th-48th layer is DEBIL. we can equivalent the ZIBRO formation with DEBIL formation.

Base on its Microfacies (Foraminifera) at end 34 Genus and 24 Species and also identity 4 assemblage of foraminifera with Deltoid diagram:

 

1. First assembly have 20% Hyaline, 40% Porcellaneous & 40% Agglutinated. Include Fallotella alavensis, Haymanella paleocenica, Idalina sinjarica, Glomalveolina primaeva, Pseudolacazina donatae, Laffitteina bibensis, Periloculina sp., Cuvillierina sp., Miscellanea miscella, Broeckinella sp.,miliolids (Quinqueloculina sp., Triloculina sp. etc.), green algae,

Upper Paleocene

 

2. Second assembly have 80% Hyaline, 15% Porcellaneous & 5% Agglutinated. Include

Nummulites with small groupscontaining N. frassi, N. partchi and N. deserti, Assilina yvettae, Rotalia sp., Nummulites globulus, Nummulites convexa, Ranikothalia sindensis, Operculina exiliformis, Operculina patalensis, Miscellanea miscella, Miscellanea sp., Ranikothalia sp. (n. s), Smoutina sp.

Upper Paleocene

 

3. Third assembly have 10% Hyaline, 60% Porcellaneous & 30% Agglutinated. Include

Sistanites iranica, Idalina sinjarica, Quinquloculina sp., Globotextularia sp.,Valvulina sp. Pseudolacazina donatae. Upper Paleocene

 

4. Forth assembly have 20% Hyaline, 50% Porcellaneous & 30% Agglutinated. Include

Alveolina aff. decipiens, Alveolina aff leupoldi, Glomalveolina cf. primaeva Triloculina sp., Quinquloculina sp., Textularia sp. pseudolacazina sp. Lower Eocene

First Assemblage Second Assemblage

Third Assemblage Forth Assemblage

 

 

Fig. Paleoenvironment and locality of Foraminifera assemblage

 

References:

 

1. Akhtar M.&A.A.Butt.1999,Microfacies and foraminiferal assemblages from the Early Tertiary rocks of the cala Chita Range (Northern Pakistan). Geologie Mediterranneene,26(3-4):185-201.

2. Alavi,M,1991:Sedimentary and structural characteristics of the paleo-Tethys remnants in northeastern Iran.Geol.Soc.Of Amer.Bull.V.103,pp.983-992.

3. Babazadeh,S.A.2003,Biostratigraphyie et controles paleogeographiques de la zone de suture de IIran oriental. Implications sur la fermeture Tethysienne.These de doctorat,Universite d’Orleans,France,384p.

4. Babazadeh,S.A.2004,Litho – biostratigraphy of Paleogene sedimentary succesion in Sahlabad province (South Birjand) and evolution on Neo – Tethyan basin closure. Scientific project,No.08/1896,1-45.

5. Babazadeh,S.A.2008,Lower Eocene transgressive successions of Sahlabad province, eastern Iran, implication of biostratigraphy and microfacies analysis, Revue de Paleobiologie, Geneve,27(2):1-11

6. Beavington-Penney,S.J.and A.Racey,2004,Ecology of extant Nummulitids and other larger benthic foraminifera application in Palaeonvironmental analysis:earth science,v.67,p.219-265.

7. Berberian,M,et al,1983:The southern Caspian,a compressional depresson floored by a trapped,modifisd volcanologique,40(2),pp.121-123.

8. Brasier,M.D.,1975d,an outline history of seagrass comunities.paleontology 18,681-702.

9. Cosovic,v.k.Drobne,and A.Moro,2004,Palaeoenvironmental model for Eocene foraminiferal limestone of the Adriatic carbonate platform(Island peninsula):facies,no.50,p.61-75.

10. Flugel,E.,2004,Microfacies of carbonate

11. Loeblich,A.R.and H. Tappan,1998,Foraminiferal genera and their classification:van Nostrand Reinhold Company,New York,970p.

12. Pomar,L.2001b,Types of carbonate platforms:a genetic approach:Basin Res.,v.13,p.313-334.

13. Romero,J.,E.Caus & J.Rosell.2002,A model for the palaeoenvironmental distribution of larger foraminifera based on late Middle Eocene deposits on the margin of the South Pyrenean basin(NE spain).Palaeogeography.Palaeoclimatology,Palaeoecology,179:43-56.

14. Romero,J.,E.Caus & J.Rosell,2004,Ecology of extant nummulitids and other larger benthic foraminifera: applications in palaeoenvironmental analysis,Earth-Science Reviews 67,p.219-265.

15. Schlager, W. (1992). Sedimentology and sequence stratigraphy of reefs and carbonate

 

 


Дата добавления: 2015-10-29; просмотров: 226 | Нарушение авторских прав


Читайте в этой же книге: Active Horsetail Splay Structure in the Cenozoic Magmatic arc of Iran | Heat Flow and Geodynamics of the Kaapvaal Craton and its implications on the potential of Enhanced Geothermal Energy in South Africa | Navab anticline: a contractional structure in the transpressive bend of Qom-Zefreh fault zone, west of central Iran | Mesozoic-Cenosoic North Kazakhstan tectonic activation, evidence by apatite fission track analyses | Complexity and Changing Pattern of Tectonics in Hydrocarbon Bearing Basin of South East Asia | Kola Peninsula | Chah-e Deev: a model of sinkholes development in center of Iranian Plateau | GEOMORPHOLOGY AND QUARTERNARY GEOLOGY | V.S. Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russia | Grain-size record of the Late Pleistocene loess deposits in the south of West Siberia |
<== предыдущая страница | следующая страница ==>
Structure of the upper part of subaeral cover of Biya-Chumysh plateau| A newly discovered Ediacaran biota containing Arkarua-like fossils from the Irkineeva Uplift, East Siberia

mybiblioteka.su - 2015-2024 год. (0.006 сек.)