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master's thesis
Seizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa
diplomski rad
Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. urn:nbn:hr:169:796180
Arandia-Krešić, Dario
University of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
Department of Geology and Geological Engineering

Institutional repository: Faculty of Mining, Geology and Petroleum Engineering Repository, University of Zagreb

Cite this document

Arandia Krešić, D. (2018). Seizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa : diplomski rad (Master's thesis). Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering. Retrieved from https://urn.nsk.hr/urn:nbn:hr:169:796180

Arandia Krešić, Dario. "Seizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. https://urn.nsk.hr/urn:nbn:hr:169:796180

Arandia Krešić, Dario. "Seizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa : diplomski rad." Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, 2018. https://urn.nsk.hr/urn:nbn:hr:169:796180

Arandia Krešić, D. (2018). 'Seizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa : diplomski rad', Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, accessed 23 November 2024, https://urn.nsk.hr/urn:nbn:hr:169:796180

Arandia Krešić D. Seizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa : diplomski rad [Master's thesis]. Zagreb: University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering; 2018 [cited 2024 November 23] Available at: https://urn.nsk.hr/urn:nbn:hr:169:796180

D. Arandia Krešić, "Seizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa : diplomski rad", Master's thesis, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb, 2018. Available at: https://urn.nsk.hr/urn:nbn:hr:169:796180

Metadata
TitleSeizmostratigrafske jedinice pliocenskih naslaga u jadranskom podmorju južno od Visa : diplomski rad
Title (english)Pliocene seismostratigraphic units in the Adriatic offshore, south of the Vis island : master’s thesis
AuthorDario Arandia-Krešić
MentorBruno Saftić (mentor)
Committee memberBruno Saftić (predsjednik povjerenstva)
Committee memberBruno Tomljenović (član povjerenstva)
Committee memberMarko Cvetković (član povjerenstva)
GranterUniversity of Zagreb
Faculty of Mining, Geology and Petroleum Engineering
(Department of Geology and Geological Engineering)
Zagreb
Defense date and country2018-04-20, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Geology
Geology and Paleontology
Abstract
Na temelju seizmičkih i bušotinskih podataka na području jadranskog podmorja južno od Visa, korištenjem programskog paketa Petrel, definirane su strukturne karte krovine miocenskog i krovine pliocenskog slijeda naslaga u vremenskom mjerilu. Seizmostratigrafskom interpretacijom između ovih strukturnih površina proučeni su stratigrafski odnosi stijena pliocenske starosti u kojima je izdvojeno pet sekvencijskih granica tipa 1 (nazvane granice a, b, c, d, i e) kojima su definirane podinske i krovinske granice četiriju seizmostratigrafskih jedinica – A, B, C i D. Izrađene su strukturne karte po navedenim stratigrafskim granicama u vremenskom mjerilu kao i karte debljina izdvojenih jedinica u vremenskom mjerilu. S obzirom na dobivene rezultate potvrđuje se da nakon taloženja sekvencije A tijekom donjeg-srednjeg pliocena dolazi do regionalne promjene taložnih uvjeta u gornjem pliocenu, i to postupno od taloženja na vanjskom šelfu do taloženja na srednjem i unutarnjem šelfu. Ova promjena se reflektira u progradaciji gornjopliocenskih sedimenata koji čine sekvencije B, C i D, sa sjevernog ruba kartiranog područja prema jug-jugozapadu.
Abstract (english)
Based on seismic and well data of Adriatic offshore area south of Vis island, tops of the Miocene and Pliocene age rocks were mapped using PetrelTM software package. Seismostratigraphic interpretation of Pliocene rock interval is based primarily on the five type 1 sequence stratigraphic boundaries named – a, b, c, d and e. The first four of these boundaries represent the base surfaces of four new seismostratigraphic sequences named A, B, C and D, while e is the top of sequence D and equals the top of Pliocene sediments. The reconstruction of the of these units is based on time-depth maps. The thickness of sequences was mapped in two-way time scale, as well as their boundary surfaces. As a result of this study it was concluded that after the sedimentation of sequence A in outer shelf environment during the Lower-Middle Pliocene, a shallowing event occurs at the beginning of Upper Pliocene. As indicated by B, C and D sequences, sedimentation is characterized by gradual progradation of the middle and inner shelf sediments from the northern edge of the mapped area towards the south-southwest.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:169:796180
Study programmeTitle: Geology; specializations in: Geology of mineral resources and geophysical explorations
Course: Geology of mineral resources and geophysical explorations
Study programme type: university
Study level: graduate
Academic / professional title: magistar/magistra geologije (magistar/magistra geologije)
Type of resourceText
File originBorn digital
Access conditionsOpen access
Terms of useLicence In copyright icon
Created on2018-06-15 13:06:09