Show/Hide Menu
Hide/Show Apps
Logout
Türkçe
Türkçe
Search
Search
Login
Login
OpenMETU
OpenMETU
About
About
Open Science Policy
Open Science Policy
Open Access Guideline
Open Access Guideline
Postgraduate Thesis Guideline
Postgraduate Thesis Guideline
Communities & Collections
Communities & Collections
Help
Help
Frequently Asked Questions
Frequently Asked Questions
Guides
Guides
Thesis submission
Thesis submission
MS without thesis term project submission
MS without thesis term project submission
Publication submission with DOI
Publication submission with DOI
Publication submission
Publication submission
Supporting Information
Supporting Information
General Information
General Information
Copyright, Embargo and License
Copyright, Embargo and License
Contact us
Contact us
GEOCHEMICAL CHARACTER OF THE HYDROTHERMAL ALTERATION ZONES AROUND THE MADENKOY-SIIRT MASSIVE SULFIDE DEPOSIT AND IMPLICATIONS FOR GEOCHEMICAL-EXPLORATION
Date
1989-04-01
Author
ERLER, A
Metadata
Show full item record
This work is licensed under a
Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License
.
Item Usage Stats
205
views
0
downloads
Cite This
The Madenkoy-Siir region lies in southeastern Anatolia, Turkey to the northeast of Siirt. The study area is in the southeastern Anatolian Thrust Belt, which forms the boundary between the Border Folds on the northern edge of the Arabian plate and the Taurids. In the region, limestones of the Midyat Group of Eocene-Miocene age and alternating marls and sandstones of the Lice Formation of Early-Middle Miocene age are the autochthonous units. Three thrust slices were emplaced over the autochthonous units during the Miocene Epoch. The lowest slice consists of interbedded sandstones, mudstones, marls, limestones, and conglomerates of the Sason flysch, the Madenkoy spilite, and the Toptepe conglomerate, all of Eocene age; the middle slice consists of the Guleman ultramafic rocks of Cretaceous age; and the uppermost slice consists of the Bitlis metamorphic rocks of Paleozoic age.
Subject Keywords
Economic geology
,
Geochemistry and petrology
URI
https://hdl.handle.net/11511/64246
Journal
JOURNAL OF GEOCHEMICAL EXPLORATION
DOI
https://doi.org/10.1016/0375-6742(89)90083-6
Collections
Department of Geological Engineering, Article
Suggestions
OpenMETU
Core
Mineralogy, chemistry and potential utilization of clays from coal deposits in the Kutahya province, Western Turkey
Tuerkmenoglu, Asuman Guenal; Yavuz-Isik, Nurdan (Elsevier BV, 2008-12-01)
Kutahya graben is one of the largest E-W trending grabens of Western Turkey consisting of Tavsanli and Seyitomer sub-basins filled with Neogene continental deposits. These deposits contain economic lignite seams and the clay samples investigated in this study are closely related to the commercial lignite deposits since they occur underlying or overlying the major coal seams and also intercalated with them.
Tectonic evolution of the Gediz Graben: field evidence for an episodic, two-stage extension in western Turkey
Bozkurt, Erdin (Cambridge University Press (CUP), 2004-01-01)
Western Turkey is one of the most spectacular regions of widespread active continental extension in the world. The most prominent structures of this region are E-W-trending grabens (e.g. Gediz and Buyuk Menderes grabens) and intervening horsts, exposing the Menderes Massif. This paper documents the result of a recent field campaign (field geological mapping and structural analysis) along the southern margin of the modern Gediz Graben of Pliocene (similar to 5 Ma) age. This work provides field evidence that ...
Hydrothermal alteration products in the vicinity of the Ahirozu kaolin deposits, Mihaliccik-Eskisehir, Turkey
Sayit, Isil Omeroglu; Günal Türkmenoğlu, Asuman; Sayin, S. Ali; Demirci, Cengiz (Mineralogical Society, 2018-06-01)
The mineralogy, texture and composition of rocks associated with the kaolin deposits in the Ahirozu-Hamidiye-Ucbasli area, SE of Mihaliccik, Eskisehir, Turkey, were investigated. In the study area, Triassic, blue-green schists and serpentinized ultramafic rocks are exposed. Kaolinization occurs at the contact between a Triassic granitic intrusion and metamorphic rocks. Textural and mineralogical characteristics were identified by X-ray diffraction (XRD) and scanning electron microscopy-energy dispersive X-r...
Spatial variations of active stress patterns and frequencymagnitude distribution of earthquakes in Western Anatolia, Turkey
Shah, S Tanvir; Özacar, Atilla Arda (null; 2018-04-23)
Western Anatolia is one of the most important tectonic elements of Turkey, and constitutes the eastern margin of Aegean Extensional Province. The area is one of the most seismically active continental margins around the globe experiencing N-S extension. Earthquake data in this study is used to analyze the active stress patterns and to estimate the earthquake return periods for different sub-regions in western Anatolia. Focal mechanism solution data is used for determining the orientations and ratios of prin...
Tectono-stratigraphic evolution of the continental miocene basins in Southwest Anatolia
Koç, Ayten; Kaymakcı, Nuretdin; Van Hinsbergen, Douwe J. J.; Department of Geological Engineering (2013)
The Tauride range in southern Turkey is flanked and overlain by Neogene sedimentary basins. To the south and on top of the high range, these basins are mainly marine, whereas poorly studied intra-montane basins dominated by continental deposits are exposed to the north. In this study, the stratigraphy and structure of these continental basins which includes Altınapa, Yalvaç and Ilgın Basins are studied. Their stratigraphy of these basins displays poorly expressed fining upwards sequences of fluvio-lacustrin...
Citation Formats
IEEE
ACM
APA
CHICAGO
MLA
BibTeX
A. ERLER, “GEOCHEMICAL CHARACTER OF THE HYDROTHERMAL ALTERATION ZONES AROUND THE MADENKOY-SIIRT MASSIVE SULFIDE DEPOSIT AND IMPLICATIONS FOR GEOCHEMICAL-EXPLORATION,”
JOURNAL OF GEOCHEMICAL EXPLORATION
, pp. 405–407, 1989, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/64246.