کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
5786688 1640775 2017 12 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
The Calabrian in the Western Transcaucasian basin (Georgia): Paleomagnetic constraints from the Gurian regional stage
ترجمه فارسی عنوان
کالابری در حوضه غربی قزاق غربی (گرجستان): محدودیت های پالموژنتیک از مرحله منطقه ای گوریان
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات زمین شناسی
چکیده انگلیسی


- A Magnetostratigraphic framework of the Gurian local stage in Georgia is established.
- Polarity pattern yields highly varying sedimentation rates within the Gurian sections.
- Paleomagnetic results reveal also vertical axis rotation between 6 and 2 Ma.
- There is magnetomineralogic evidence for a shift from greigite to magnetite sedimentation.

The precise Eurasian chronostratigraphy of the Neogene-Quaternary period is still hampered by the existence of numerous regional stages often lacking independent and absolute age constraints. Therefore, detailed paleoclimatic reconstructions of areas like the Caucasus are still poorly constrained and the influence of climate variability on faunal interchange between Africa and Eurasia in the late Neogene-Quaternary is still difficult to address. During the last decades, Quaternary sections from western Georgia have produced a wealth of paleoclimatic proxy data. Unfortunately, these sections do not have a robust age control. This is especially true for the Gurian stage which has been vaguely defined as being coeval with the lower Pleistocene on the basis of poorly documented bio- and magnetostratigraphic data. In order to constrain the age of the Gurian stage, a detailed magnetostratigraphic study has been carried out. All major sections with known Gurian sediments in the former Rioni bay (a marine restricted area to the southeast of the Major Caucasus) have been studied. Our results confirm for the first time the strict correlation between the Gurian succession and the Calabrian stage.In addition, our data provides further information on the tectonic setting of the Rioni bay during the Calabrian in this region: (1) in the north, Gurian sediments were unconformably deposited on older Meotian sediments in a piggy back basin, (2) in the south, Gurian sediments are conformably overlying Kujalnician (Plio-Pleistocene) strata, (3) magnetostratigraphic correlation among sections indicate drastic changes in sediment accumulation rates within the basin, (4) rock magnetic experiments reveal significant magnetomineralogical differences between Gurian and the underlying Miocene sediments likely documenting a transition related to changes in oxic conditions, supply of terrigenous material and sedimentation rate close to the Miocene-Pliocene boundary.These results provide a robust basis for further tectonic and paleoclimatic investigations of this region.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Quaternary Science Reviews - Volume 160, 15 March 2017, Pages 96-107
نویسندگان
, , , , , ,