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![Figure 3. (A) Uppermost Tithonian section from Lastovo Island (section LSL; Fig. 1) showing facies stacking, parasequences, and parasequence sets. Upward-deepening units are shown by upward-narrowing triangle; upward-shallowing units are shown by upward-widening triangle. (B) Details of portion of measured section showing location of oolitic units within parasequences. (C) Idealized succession of facies within an Upper Tithonian parasequence. M—lime mudstone, W—wackestone, P—packstone, G—grainstone, F—floatstone, R—rudstone.]()
![Figure 1. (A) Map of south-central Europe showing location of Adriatic Platform (modified from Grandić et al., 1999; Velić et al., 2002). Rectangle shows area enlarged in B. (B) Location of the studied section on Lastovo Island (LSL).]()
![Geologic map of the central Adriatic region showing the front of the thin-skinned thrust belt and the late orogenic northwest-southeast–trending dextral Adriatic strike-slip fault system (AFS). Also shown are the associated compressional anticlinal structures bounded by sinistral strike-slip faults in the island area between Split (S) and Dubrovnik (D) and the location of deep anticlinal structures Boka Kotorska (BK) and Ulcinj (U). The Albanian foredeep evolved on top of the Ionian Mesozoic basin. The isopachs show the total thickness of the basin fill, including both the foredeep and the pull-apart stages. B = Brac Island; H = Hvar Island; K = Korcula Island; L = Lastovo Island; M = Mljet Island; P = Peljesac Peninsula; T = Tirana. Reprinted from Picha (2002) with permission from AAPG.]()
![Outcrop photographs of lithofacies. A) Upper Tithonian early diagenetic dolomite with well-preserved laminated texture of stromatolitic origin, Mljet Island. B) Berriasian emersion breccia with clasts of predominantly lime mudstone and fenestral limestone, Lastovo Island. C) Approximately 2-m-thick Barremian interval with clasts of brecciated and corroded lime mudstone and peloidal mudstone–wackestone embedded in a greenish-grayish clay matrix, Mljet Island. D) Emersion breccia with clasts of Upper Aptian limestones, Korčula Island. E) Upper Aptian subaerial exposure interval with grayish-greenish clayey–marly material, Pelješac Peninsula. F) Albian alternation of thin beds and laminae of dark, dolomitized limestones containing kerogen and light-gray mudstones, Korčula Island. G) Upper Albian–Lower Cenomanian dolomitized stromatolitic laminite, Mljet Island. H) Polygonal desiccation cracks in Cenomanian limestone, Mljet Island. Objects for scale: hammer (32.8 cm long), lens cap (52 mm in diameter), magnifier lens (20 mm in diameter), and coin (22 mm in diameter).]()
![Figure 4. Thin-section photomicrographs of typical Upper Jurassic (Tithonian) ooid grainstone composed of large, whole and fragmented-and-recoated radial ooids, Lastovo Island, Croatia. Bar scale is 1 mm. (A) Typical ooid grainstone facies. (B) Large fenestral pore (f) developed within ooid grainstone. Meniscus cements shown by arrows. (C) Ooids bound together by micritic meniscus cements (arrows). (D) Broken radial ooids showing little or no abrasion, coated with radial envelopes. (E) Ooid (center) characterized by cerebroid outlines with well-developed radial structure, and lesser-developed concentric laminae of micritized carbonate. (F and G) Small clusters of whole and fragmented ooids forming grapestone-like aggregates coated with radial calcite laminae. (H) Hardground and contact of skeletal (Campbelliella) wackestone and ooid grainstone.]()
![Photomicrographs of important rock types. A) Tithonian oncoidal ("algal ball") floatstone, Mljet Island (Ogiran Islet). Quiet, low-energy lagoonal setting below the zone of frequent wave reworking. B) Upper Tithonian ooid grainstone with meniscus micrite cements, Lastovo Island. Shallow subtidal–intertidal shoal or pond. C) Hauterivian ooid grainstone with meniscus micrite cements, Mljet Island. Shallow subtidal–intertidal shoal or pond. D) Laminated alternation of Barremian mudstone, fenestral mudstone and cryptalgal laminite, Mljet Island. Intertidal–supratidal setting with thin microbial mat covers. E) Lower Aptian skeletal mudstone-wackestone with foraminifer Palorbitolina lenticularis, Korčula Island. Quiet, low-energy lagoonal setting below the zone of frequent wave reworking. F) Upper Aptian peloidal–skeletal wackestone–packstone with numerous sections of the alga Salpingoporella dinarica, Mljet Island. Low-energy setting, shallow lagoon. G) Dark, organic-rich, mud-supported dolomitized Upper Albian limestone with charophytes, Korčula Island. Probably lacustrine or brackish environment. H) Laminated Upper Albian to Lower Cenomanian early diagenetic dolomite, Mljet Island. Intertidal–supratidal setting.]()
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![Map of central and southern Adriatic region showing the front of the Dinaric thin-skinned thrust belt and the late orogenic northwest-southeast-trending, right-lateral Adriatic strike-slip fault system (AF). Genetically associated with the major strike-slip faults are both the en echelon fault-bounded anticlinal structures, evident from the pattern of islands in the area between Split (S) and Dubrovnik (D) and the Pliocene-Quaternary Albanian foredeep interpreted as a pull-apart basin. Also shown is the location of seismic line 28, cross sections AA' and BB', and the deep structures Boka Kotorska (BK) and Ulcinj (U). B = Brac; H = Hvar; K = Korcula; L = Lastovo; M = Mljet; P = Peljesac; T = Tirana.]()
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Lastovo Island
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Image
Figure 3. (A) Uppermost Tithonian section from Lastovo Island (section LSL;... Available to Purchase
in Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters
> GSA Bulletin
Published: 01 May 2006
Figure 3. (A) Uppermost Tithonian section from Lastovo Island (section LSL; Fig. 1 ) showing facies stacking, parasequences, and parasequence sets. Upward-deepening units are shown by upward-narrowing triangle; upward-shallowing units are shown by upward-widening triangle. (B) Details of portion
Image
Figure 1. (A) Map of south-central Europe showing location of Adriatic Plat... Available to Purchase
in Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters
> GSA Bulletin
Published: 01 May 2006
Figure 1. (A) Map of south-central Europe showing location of Adriatic Platform (modified from Grandić et al., 1999 ; Velić et al., 2002 ). Rectangle shows area enlarged in B. (B) Location of the studied section on Lastovo Island (LSL).
Image
Geologic map of the central Adriatic region showing the front of the thin-s... Available to Purchase
in Late orogenic faulting of the foreland plate: An important component of petroleum systems in orogenic belts and their forelands
> AAPG Bulletin
Published: 01 June 2011
and the pull-apart stages. B = Brac Island; H = Hvar Island; K = Korcula Island; L = Lastovo Island; M = Mljet Island; P = Peljesac Peninsula; T = Tirana. Reprinted from Picha (2002) with permission from AAPG.
Image
Outcrop photographs of lithofacies. A) Upper Tithonian early diagenetic d... Available to Purchase
in Relative Sea-Level Changes Recorded on an Isolated Carbonate Platform: Tithonian to Cenomanian Succession, Southern Croatia
> Journal of Sedimentary Research
Published: 01 October 2006
Figure 7 Outcrop photographs of lithofacies. A) Upper Tithonian early diagenetic dolomite with well-preserved laminated texture of stromatolitic origin, Mljet Island. B) Berriasian emersion breccia with clasts of predominantly lime mudstone and fenestral limestone, Lastovo Island. C
Image
Figure 4. Thin-section photomicrographs of typical Upper Jurassic (Tithonia... Available to Purchase
in Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters
> GSA Bulletin
Published: 01 May 2006
Figure 4. Thin-section photomicrographs of typical Upper Jurassic (Tithonian) ooid grainstone composed of large, whole and fragmented-and-recoated radial ooids, Lastovo Island, Croatia. Bar scale is 1 mm. (A) Typical ooid grainstone facies. (B) Large fenestral pore (f) developed within ooid
Image
Photomicrographs of important rock types. A) Tithonian oncoidal ("algal b... Available to Purchase
in Relative Sea-Level Changes Recorded on an Isolated Carbonate Platform: Tithonian to Cenomanian Succession, Southern Croatia
> Journal of Sedimentary Research
Published: 01 October 2006
Figure 6 Photomicrographs of important rock types. A) Tithonian oncoidal ("algal ball") floatstone, Mljet Island (Ogiran Islet). Quiet, low-energy lagoonal setting below the zone of frequent wave reworking. B) Upper Tithonian ooid grainstone with meniscus micrite cements, Lastovo Island
Journal Article
Transgressive oversized radial ooid facies in the Late Jurassic Adriatic Platform interior: Low-energy precipitates from highly supersaturated hypersaline waters Available to Purchase
Journal: GSA Bulletin
Publisher: Geological Society of America
Published: 01 May 2006
GSA Bulletin (2006) 118 (5-6): 550–556.
...Figure 3. (A) Uppermost Tithonian section from Lastovo Island (section LSL; Fig. 1 ) showing facies stacking, parasequences, and parasequence sets. Upward-deepening units are shown by upward-narrowing triangle; upward-shallowing units are shown by upward-widening triangle. (B) Details of portion...
FIGURES
Journal Article
Relative Sea-Level Changes Recorded on an Isolated Carbonate Platform: Tithonian to Cenomanian Succession, Southern Croatia Available to Purchase
Journal: Journal of Sedimentary Research
Publisher: SEPM Society for Sedimentary Geology
Published: 01 October 2006
Journal of Sedimentary Research (2006) 76 (10): 1120–1136.
...Figure 7 Outcrop photographs of lithofacies. A) Upper Tithonian early diagenetic dolomite with well-preserved laminated texture of stromatolitic origin, Mljet Island. B) Berriasian emersion breccia with clasts of predominantly lime mudstone and fenestral limestone, Lastovo Island. C...
FIGURES
Image
Map of central and southern Adriatic region showing the front of the Dinari... Available to Purchase
in Late Orogenic Strike-Slip Faulting and Escape Tectonics in Frontal Dinarides-Hellenides, Croatia, Yugoslavia, Albania, and Greece
> AAPG Bulletin
Published: 01 September 2002
fault-bounded anticlinal structures, evident from the pattern of islands in the area between Split (S) and Dubrovnik (D) and the Pliocene-Quaternary Albanian foredeep interpreted as a pull-apart basin. Also shown is the location of seismic line 28, cross sections AA' and BB', and the deep structures
Journal Article
Late Orogenic Strike-Slip Faulting and Escape Tectonics in Frontal Dinarides-Hellenides, Croatia, Yugoslavia, Albania, and Greece Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 September 2002
AAPG Bulletin (2002) 86 (9): 1659–1671.
... fault-bounded anticlinal structures, evident from the pattern of islands in the area between Split (S) and Dubrovnik (D) and the Pliocene-Quaternary Albanian foredeep interpreted as a pull-apart basin. Also shown is the location of seismic line 28, cross sections AA' and BB', and the deep structures...
FIGURES
Journal Article
Geologic-Tectonic Structure and Evolution of Outer Dinarides and Adriatic Area Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 May 1973
AAPG Bulletin (1973) 57 (5): 913–929.
... eugeosynclinal area and intergeosynclinal zone and massif, mostly in the form of islands. In Figure 1 a black rectangle outlines the Outer Dinarides and the Adriatic area which were studied in great detail. The basic results obtained are discussed in this paper. The Adriatic shelf is composed mainly...
FIGURES
Journal Article
The Adriatic Thrust Fault of the 2021 Seismic Sequence Estimated from Accurate Earthquake Locations Using sP Depth Phases Available to Purchase
Publisher: Seismological Society of America
Published: 02 December 2022
Bulletin of the Seismological Society of America (2023) 113 (1): 480–493.
..., aligned along the northwest–southeast direction, are shown in Figure 1 . The mainshock of the 2021 seismic sequence occurred approximately 20 km north of the Palagruza Islands, 80 km from the Gargano promontory, and approximately 40 km from the Croatian island of Lastovo. This mainshock was felt...
FIGURES
Includes: Supplemental Content
Journal Article
Late orogenic faulting of the foreland plate: An important component of petroleum systems in orogenic belts and their forelands Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 June 2011
AAPG Bulletin (2011) 95 (6): 957–981.
... and the pull-apart stages. B = Brac Island; H = Hvar Island; K = Korcula Island; L = Lastovo Island; M = Mljet Island; P = Peljesac Peninsula; T = Tirana. Reprinted from Picha (2002) with permission from AAPG. ...
FIGURES
Journal Article
Petroleum Exploration and Production in Europe in 1969 Available to Purchase
Journal: AAPG Bulletin
Publisher: American Association of Petroleum Geologists
Published: 01 August 1970
AAPG Bulletin (1970) 54 (8): 1407–1456.
... Sea and south to the Montenegran coast. It was planned to spud an exploratory well in early 1970 on the Adriatic Island of Lastovo, where the Paleocene was believed to offer favorable prospects. Production of oil in the Soviet Union in 1969 was 328 million m. t. (2.3 billion bbl) (up 6% from...
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