Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Ali UÇURUM"'
Publikováno v:
Bulletin of the Mineral Research and Exploration, Vol 141, Iss 141, Pp 27-52 (2010)
Pınarbaşı Apatitli Manyetit Yatağı'nın yakın çevresinde, alttan üste doğru klorit, serisit ve kalkşistlerle re- kristalize kireçtaşlarından oluşan Permiyen yaşlı Malatya Metamorfitleri vardır. Eosen yaşlı Maden Karmaşığı'nın
Externí odkaz:
https://doaj.org/article/da4461b30ddb4ff9b66eaa1a62615c6b
Publikováno v:
Volume: 22, Issue: 4 215-237
Kahramanmaraş Sütçü İmam Üniversitesi Mühendislik Bilimleri Dergisi
Kahramanmaraş Sütçü İmam Üniversitesi Mühendislik Bilimleri Dergisi
Sölestin içeren evaporitler Sivas Tersiyer Havzasında yaygındır. Sivas bölgesinde Akkaya sölestin yatağı en eski ve en büyük açık işletme olup Eosen yaşlıdır ve masif cevher içermektedir.Evaporit minerallerin δD ve δ18 O verilerin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::adfa145e635ca458f82985d2dc43a557
https://dergipark.org.tr/tr/pub/ksujes/issue/51076/657193
https://dergipark.org.tr/tr/pub/ksujes/issue/51076/657193
Autor:
Ali Uçurum, Taner Ekici, Joaquin Ruiz, Ryan Mathur, Jason Kirk, Cigdem Sahin Demir, Mustafa Erturk, Nazmi Otlu, Greg B. Arehart
Publikováno v:
Minerals
Volume 11
Issue 2
Minerals, Vol 11, Iss 226, p 226 (2021)
Volume 11
Issue 2
Minerals, Vol 11, Iss 226, p 226 (2021)
The eastern Pontide tectonic belt (EPTB) contains greater than 350 identified Kuroko type volcanogenic massive sulfide deposits/mineralization/occurrences (VMSD). The deposits are associated with Late Cretaceous felsic volcanics consisting mainly of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::914ca864a6a95920418bf16e9e49498e
https://doi.org/10.3390/min11020226
https://doi.org/10.3390/min11020226
Autor:
Ali Uçurum, Cigdem Sahin Demir
Publikováno v:
Türkiye Jeoloji Bülteni / Geological Bulletin of Turkey. 59:87-114
Bu çalışma Evliya Tepe yakınında Güzelyurt köyü Sisorta bölgesindeki altın yatağının jeolojik ve jeokimyasal özelliklerini sunmaktadır. Çalışma alanı 42 km2'lik alanı kapsamakta ve Sivas'ın 200 km KB'da Sisorta'dadır.Sisorta alt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c59116a7507e4d90883158ef096bd0f5
https://doi.org/10.25288/tjb.298300
https://doi.org/10.25288/tjb.298300
Publikováno v:
Journal of Scientific Research and Reports. 4:348-374
The Precambrian (Puturge Metamorphites), the Eocene (Maden Complex), the Permo- Carboniferous (Malatya Metamorphites), the tertiary conglomerates and the alluvial formation all crop out in the vicinity of the magnetite-apatite ore deposits of Pinarba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42a84b688d2a8b912ecbc6fcaac0a1d7
https://doi.org/10.9734/jsrr/2015/9793
https://doi.org/10.9734/jsrr/2015/9793
Publikováno v:
International Geology Review. 49:753-767
The Bakir Tepe area is characterized by four different lithologic units of Devonian-Carboniferous age. These units, from bottom to top, are metasiltstone, metacarbonate, metasandstone, and metaquartz sandstone. Metamorphic rocks in the study area are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bb98efb078955420c5ac1b65a94ca52b
https://doi.org/10.2747/0020-6814.49.8.753
https://doi.org/10.2747/0020-6814.49.8.753
Publikováno v:
International Geology Review. 49:169-192
WOS: 000243389800004
Cunes-Sogucak Ni-Cu-sulfide mineralization in the Divrigi district of Sivas Province is genetically related to I.ate Cretaceous ultramafie rocks. Disseminated mineralization is scattered through the ultramafic rocks, whereas
Cunes-Sogucak Ni-Cu-sulfide mineralization in the Divrigi district of Sivas Province is genetically related to I.ate Cretaceous ultramafie rocks. Disseminated mineralization is scattered through the ultramafic rocks, whereas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9d38960813dfb216cf503efe3d4be0f8
https://doi.org/10.2747/0020-6814.49.2.169
https://doi.org/10.2747/0020-6814.49.2.169
Autor:
Ali Uçurum
Publikováno v:
Volume: 7, Issue: 2 87-96
Turkish Journal of Earth Sciences
Turkish Journal of Earth Sciences
Bu çalışma Divriği ve Hekimhan bölgelerindeki üç farklı listvenit mostrasından alınan örneklerin Co, Ni, As, Ag ve Au konsantrasyonları arasındaki olası ilişkiyi bulmayı amaçlamıştır. Cürek-Divriği, Sivas , Güvenç ve Karakuz-H
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::637f1a4441773c8e07ac4d73a5e58cfd
https://dergipark.org.tr/tr/pub/tbtkearth/issue/12036/143845
https://dergipark.org.tr/tr/pub/tbtkearth/issue/12036/143845
Autor:
Ali Uçurum
Publikováno v:
International Geology Review. 42:172-191
WOS: 000086073900005
The Divrigi and Kuluncak ophiolitic melanges are located in central Anatolia in the Tauride ophiolite belt. The stratigraphic sequence in the Divrigi ophiolitic melange includes, from bottom to top, the Upper Jurassic-Lower
The Divrigi and Kuluncak ophiolitic melanges are located in central Anatolia in the Tauride ophiolite belt. The stratigraphic sequence in the Divrigi ophiolitic melange includes, from bottom to top, the Upper Jurassic-Lower
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3e79f321169022773714313ad6a1e094
https://doi.org/10.1080/00206810009465076
https://doi.org/10.1080/00206810009465076
Publikováno v:
International Geology Review. 39:744-755
The Güneyocak chromite mineralization is hosted by the Upper Cretaceous Divrigi ophiolitic melange, which consists of serpentinite, serpentinized harzburgite and dunite, gabbro, diabase dikes, pyroxenite, blocks of limestone, and radiolarite. Serpen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f7e5879cc414e19b61fec37e479f9f21
https://doi.org/10.1080/00206819709465299
https://doi.org/10.1080/00206819709465299