نتایج جستجو برای: assemblage zone

تعداد نتایج: 119274  

خلیل فروزنده, رضا صادقی مهین محمدی

  این پژوهش به بررسی توالی رسوبی سازند آسماری به سن الیگوسن در برش چینه­شناسی تنگ مشکان با هدف مطالعه سنگ­چینه­نگاری، زیست­چینه­نگاری، تعیین ریزرخساره­ها، دسته­ریزرخساره­ها، زیرمحیط­ها و محیط رسوبی ­ می­پردازد. برش مذکور، در دامنه جنوبی تاقدیس تامار (زیرپهنه فارس نیمه­ساحلی) واقع در زاگرس چین­خورده و در محدوده مرزی استان­های فارس و کهگیلویه و بویراحمد انتخاب گردیده که ضخامت آن بالغ بر 350 متر ا...

2003
JACOB J. HANLEY JAMES E. MUNGALL

An assemblage of hydrous, Cl-bearing alteration-induced minerals is present within 150 m of footwall-style Cu–Ni–PGE sulfide mineralization hosted by the Sudbury Breccia at the Fraser Copper zone, Fraser mine, Onaping–Levack area, Ontario. The pyroxene hornfels to hornblende hornfels contact-metamorphic aureole of the Sudbury Igneous Complex (SIC) contains less than 15 modal % hydroxysilicates....

2015
Benjamin P. Horton John W. Murray

We have collected live and dead foraminiferal times-series data at 2-weekly intervals for a 12-month period from the intertidal zone of Cowpen Marsh, Tees Estuary, UK. The data from the 689 samples show profound differences between live and dead assemblages, although assemblages are dominated by just three species, Haynesina germanica, Jadammina macrescens and Trochammina inflata, which represe...

2007
SPENCER G. LUCAS MICHAEL J. ORCHARD

The Triassic section north of Currie in southern Elko County, Nevada, is almost 500 m thick and is assigned to the Thaynes Group and overlying Shinarump Formation of the Chinle Group. The Thaynes Group disconformably overlies the Permian Gerster Formation and is mostly calcareous shale with interbedded wackestones that yield marine invertebrate fossils, especially ammonoids. The Shinarump Forma...

1984
Paul E. Olsen

The Molteno, Elliot, and Clarens formations comprise the continental Stormberg Group of the Karoo Basin of South Africa and Lesotho. The Molteno Formation contains a well preserved macroand microfloral assemblage but apparently no vertebrates; the Elliot and Clarens formations contain abundant vertebrates but virtually no floral remains. The vertebrate taxa represented by skeletal remains are l...

2015
Crystal M. Ernst Christopher M. Buddle

Many macroecological patterns of biodiversity, including the relationship between latitude and species richness, are well-described. Data collected in a repeatable, standardized manner can advance the discipline beyond the description of patterns and be used to elucidate underlying mechanisms. Using standardized field methods and a hyper-diverse focal taxon, viz. Coleoptera, we aim to (1) descr...

2008
Robert B. Howard

Associate Professor of Geomorphology, Department of Geography, California State University, Northridge. Abstract: Dividing exogenic processes into constituents enables one to distinguish between denudational and depositional environments. This distinction leads to the recognition that the chaparral assemblage occupies a zone which is predominantly denudational. A qualitative assessment of sane ...

2009
JUAN CARLOS CISNEROS AKIKO TSUJI

The Middle Permian Tapinocephalus Assemblage Zone in South Africa has produced a rich record of tetrapods domi− nated by dinocephalian therapsids and pareiasaurid para− reptiles. In this study we reassess the affinities of a specimen from this horizon previously identified as a procolophonoid and provide evidence that it is instead referable to a nyctero− leter parareptile, an identification th...

Journal: :iranian journal of science and technology (sciences) 2014
j. izadyar

for the first time, an unusual assemblage of talc-phengite-chlorite-k-feldspar was found in quartz schists from the sanandaj-sirjan zone in the nahavand area in western iran. the talc-bearing quartz schists occur as small bodies or lenses within pelitic schist layers and contain talc, phengite, chlorite, k-feldspar and quartz as major mineral constituents with subordinate amounts of calcite ...

Abedini, Ali, Afkhami Nahand, Adel, Alipour, Samad, Zakeri, Laila,

Intrusion of granodioritic and quartz-dioritic igneous bodies of the Oligocene age into andesitic rocks with the Eocene age resulted in occurrence of widespread argillic alteration zone in the Asbkhan area of Heris (East Azerbaijan Province, NW Iran). A significant portion of this system formed the argillic alteration zone. Based on mineralogical examinations, kaolinite, quartz, smectite, aluni...

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