H. KORAL Et Al. , "ORTA SAKARYA (GÖYNÜK-BEYPAZARI) TERSİYER İSTİFİNİN TEKTONOSTRATİGRAFİK ÖZELLİKLERİ / TECTONO-STRATIGRAPHICAL FEATURES OF THE TERTIARY SEQUENCE IN THE CENTRAL SAKARYA BELT (GÖYNÜKBEYPAZARI)," 71. TÜRKİYE JEOLOJİ KURULTAYI , Ankara, Turkey, pp.59-60, 2018
KORAL, H. Et Al. 2018. ORTA SAKARYA (GÖYNÜK-BEYPAZARI) TERSİYER İSTİFİNİN TEKTONOSTRATİGRAFİK ÖZELLİKLERİ / TECTONO-STRATIGRAPHICAL FEATURES OF THE TERTIARY SEQUENCE IN THE CENTRAL SAKARYA BELT (GÖYNÜKBEYPAZARI). 71. TÜRKİYE JEOLOJİ KURULTAYI , (Ankara, Turkey), 59-60.
KORAL, H., KARAAĞAÇ, S., BAYKUT, T., BEHZAD, B., & İŞBİL, D., (2018). ORTA SAKARYA (GÖYNÜK-BEYPAZARI) TERSİYER İSTİFİNİN TEKTONOSTRATİGRAFİK ÖZELLİKLERİ / TECTONO-STRATIGRAPHICAL FEATURES OF THE TERTIARY SEQUENCE IN THE CENTRAL SAKARYA BELT (GÖYNÜKBEYPAZARI) . 71. TÜRKİYE JEOLOJİ KURULTAYI (pp.59-60). Ankara, Turkey
KORAL, Hayrettin Et Al. "ORTA SAKARYA (GÖYNÜK-BEYPAZARI) TERSİYER İSTİFİNİN TEKTONOSTRATİGRAFİK ÖZELLİKLERİ / TECTONO-STRATIGRAPHICAL FEATURES OF THE TERTIARY SEQUENCE IN THE CENTRAL SAKARYA BELT (GÖYNÜKBEYPAZARI)," 71. TÜRKİYE JEOLOJİ KURULTAYI, Ankara, Turkey, 2018
KORAL, Hayrettin Et Al. "ORTA SAKARYA (GÖYNÜK-BEYPAZARI) TERSİYER İSTİFİNİN TEKTONOSTRATİGRAFİK ÖZELLİKLERİ / TECTONO-STRATIGRAPHICAL FEATURES OF THE TERTIARY SEQUENCE IN THE CENTRAL SAKARYA BELT (GÖYNÜKBEYPAZARI)." 71. TÜRKİYE JEOLOJİ KURULTAYI , Ankara, Turkey, pp.59-60, 2018
KORAL, H. Et Al. (2018) . "ORTA SAKARYA (GÖYNÜK-BEYPAZARI) TERSİYER İSTİFİNİN TEKTONOSTRATİGRAFİK ÖZELLİKLERİ / TECTONO-STRATIGRAPHICAL FEATURES OF THE TERTIARY SEQUENCE IN THE CENTRAL SAKARYA BELT (GÖYNÜKBEYPAZARI)." 71. TÜRKİYE JEOLOJİ KURULTAYI , Ankara, Turkey, pp.59-60.
@conferencepaper{conferencepaper, author={Hayrettin KORAL Et Al. }, title={ORTA SAKARYA (GÖYNÜK-BEYPAZARI) TERSİYER İSTİFİNİN TEKTONOSTRATİGRAFİK ÖZELLİKLERİ / TECTONO-STRATIGRAPHICAL FEATURES OF THE TERTIARY SEQUENCE IN THE CENTRAL SAKARYA BELT (GÖYNÜKBEYPAZARI)}, congress name={71. TÜRKİYE JEOLOJİ KURULTAYI}, city={Ankara}, country={Turkey}, year={2018}, pages={59-60} }