The volcanic activity of Mt. Karacadag (SE Anatolia) is divided into three major stages: Siverek Stage (11–2.7 Ma), Karacadag Stage (1.9–1.0 Ma) and Ovabag Stage (0.4–0.01 Ma). The magmas are mildly alkaline mafic rocks, mostly basanites, hawaiites and alkali basalts. Detailed geochemical investigation indicates a continuous variation of composition with time, with the oldest products (Siverek Stage) being characterized by average lowest HFSE (Ti, Hf, Zr, Nb, Ta), 143Nd/144Nd, Nb/U, Ta/Yb, Nb/Nb and the highest DQ, La/Nb, Ti/Nb, Zr/Nb, Ba/Nb, Th/Ta, K/La, and the youngest products (Ovabag Stage) at the opposite end of the trend. The overall incompatible element content of the Karacadag volcanic rocks resembles closely average HIMU-OIB compo...
WOS: 000344525100005Mafic and felsic igneous rocks in the Karacaali Magmatic Complex (KMC) in the no...
The SE part of Turkey is characterized by a transtensional regime within the complex collision zone ...
Upper Cretaceous to Tertiary igneous rocks outcrop in the Hekimhan-Hasancelebi area, about 80 km to ...
The volcanic activity of Mt. Karacadag (SE Anatolia) is divided into three major stages: Siverek Sta...
Volcanic activity at Mt. Karacada˘g, SE Turkey, developed between 11 and 0.01 Ma. In this paper we i...
A geochemical and isotope-geochemical (Sr-Nd-Pb) study has been carried out for the Karacadag neovol...
International audienceThe Karacadag (Kulu-Konya) area is one of the main volcanic provinces in Centr...
Pliocene to Quaternary magmatism in the Karacadag Volcanic Complex in SE Turkey occurred in the fore...
A diffuse Neogene-Quaternary volcanic belt crops out in Central and Eastern Anatolia. Since the earl...
In Western Anatolia early-middle Miocene post-collisional volcanism is represented by K nch volcanic...
A diffuse and voluminous (>1400 km3) Miocene-Quaternary volcanic activity developed around the Ka...
Quaternary mafic lavas in Central Anatolia provide geochemical insights into melt generation process...
International audienceThis study is based on an integrated approach combining results from petrology...
The Karakoç Magmatic Association (KMA) within the Central Anatolian Crystalline Complex (CACC) consi...
A diffuse and voluminous (>1400 km3) Miocene-Quaternary volcanic activity developed around the Karlı...
WOS: 000344525100005Mafic and felsic igneous rocks in the Karacaali Magmatic Complex (KMC) in the no...
The SE part of Turkey is characterized by a transtensional regime within the complex collision zone ...
Upper Cretaceous to Tertiary igneous rocks outcrop in the Hekimhan-Hasancelebi area, about 80 km to ...
The volcanic activity of Mt. Karacadag (SE Anatolia) is divided into three major stages: Siverek Sta...
Volcanic activity at Mt. Karacada˘g, SE Turkey, developed between 11 and 0.01 Ma. In this paper we i...
A geochemical and isotope-geochemical (Sr-Nd-Pb) study has been carried out for the Karacadag neovol...
International audienceThe Karacadag (Kulu-Konya) area is one of the main volcanic provinces in Centr...
Pliocene to Quaternary magmatism in the Karacadag Volcanic Complex in SE Turkey occurred in the fore...
A diffuse Neogene-Quaternary volcanic belt crops out in Central and Eastern Anatolia. Since the earl...
In Western Anatolia early-middle Miocene post-collisional volcanism is represented by K nch volcanic...
A diffuse and voluminous (>1400 km3) Miocene-Quaternary volcanic activity developed around the Ka...
Quaternary mafic lavas in Central Anatolia provide geochemical insights into melt generation process...
International audienceThis study is based on an integrated approach combining results from petrology...
The Karakoç Magmatic Association (KMA) within the Central Anatolian Crystalline Complex (CACC) consi...
A diffuse and voluminous (>1400 km3) Miocene-Quaternary volcanic activity developed around the Karlı...
WOS: 000344525100005Mafic and felsic igneous rocks in the Karacaali Magmatic Complex (KMC) in the no...
The SE part of Turkey is characterized by a transtensional regime within the complex collision zone ...
Upper Cretaceous to Tertiary igneous rocks outcrop in the Hekimhan-Hasancelebi area, about 80 km to ...