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| 1 | Current concept in dysplastic hip arthroplasty: Techniques for acetabular and femoral reconstruction显示文摘Adult patients with developmental dysplasia of the hip develop secondary osteoarthritis and eventually end up with total hip arthroplasty(THA) at younger age. Because of altered anatomy of dysplastic hips, THA in these patients represents technically demanding procedure. Distorted anatomy of the acetabulum and proximal femur together with conjoined leg length discrepancy present major challenges during performing THA in patients with developmental dysplasia of the hip. In addition, most patients are at younger age, therefore, soft tissue balance is of great importance(especially the need to preserve the continuity of abductors) to maximise postoperative functional result. In this paper we present a variety of surgical techniques availablefor THA in dysplastic hips, their advantages and disadvantages. For acetabular reconstruction following techniques are described: Standard metal augments(prefabricated), Custom made acetabular augments(3D printing), Roof reconstruction with vascularized fibula, Roof reconstruction with pedicled iliac graft, Roof reconstruction with autologous bone graft, Roof reconstruction with homologous bone graft, Roof reconstruction with auto/homologous spongious bone, Reinforcement ring with the hook in combination with autologous graft augmentation, Cranial positioning of the acetabulum, Medial protrusion technique(cotyloplasty) with chisel, Medial protrusion technique(cotyloplasty) with reaming, Cotyloplasty without spongioplasty. For femoral reconstruction following techniques were described: Distraction with external fixator, Femoral shortening through a modified lateral approach, Transtrochanteric osteotomies, Paavilainen osteotomy, Lesser trochanter osteotomy, Double-chevron osteotomy, Subtrochanteric osteotomies, Diaphyseal osteotomies, Distal femoral osteotomies. At the end we present author's treatment method of choice: for acetabulum we perform cotyloplasty leaving only paper-thin medial wall, which we break during acetabular cup impacting. For femoral side first we peel of all rotators and posterior part of gluteus medius and vastus lateralis from greater trochanter on the very thin flake of bone. This method allows us to adequately shorten proximal femoral stump, with possibility of additional resection of proximal femur. Furthermore, several advantages and disadvantages of this procedure are also discussed. | Goran Bicanic Katarina Barbaric Ivan Bohacek Ana Aljinovic Domagoj Delimar | 2014 | World Journal of Orthopedics2014，5，4： | 27 |
| 2 | Stratigraphic Definition and Correlation of Middle Triassic Volcaniclastic Facies in the External Dinarides: Croatia and Bosnia and Herzegovina显示文摘Middle Triassic volcaniclastic depositsin the External Dinarides of Croatia and Bosnia and Herzegovina are related to the rifting of the Tethyan Ocean. Three localities in the External Dinarides: Donje Pazari?te, Bosansko Grahovo and Zelovo were biostratigraphically analysed in this study. The Middle Triassic carbonate deposits with volcaniclastic interlayers in Donje Pazari?te were defined by means of conodonts. Rare ammonoid specimens were collected.Recovered conodont and ammonoid taxa suggest these sections are of Early Illyrian to Early Fassanian Age. The section studied in Bosansko Grahovo is dominantly composed of volcanic and volcaniclastic rocks. Limestone peperites were collected for conodont analysis. Two conodont zones were defined, suggesting volcanic activity in the same, from Lower Illyrian to Fassanian, time interval. The Zelovo Section was biostratigraphically investigated by several authors. The pietra verde deposits from Zelovo are referred as late Fassanian to Early Longobardian Age. Biostratigraphic correlation from mentioned three localities imply that the magmatic activity in the External Dinarides, and formation of different volcaniclastic facies lasted from Illyrian to Longobardian, similar as in the surrounding western Tethyan territories. | Duje Smircic Tea Kolar-Jurkovsek Dunja Aljinovic Uros Barudzija Bogdan Jurkovsek Hazim Hrvatovic | 2018 | Journal of Earth Science2018，29，4： | 2 |
| 3 | Methylmalonic acidemia:a megamitochondrial disorder affecting the kidney显示文摘 | Zsengeller ZK Aljinovic N Teot L A | 2014 | Pediatr Nephrol2014，29，11： | 1 |
| 4 | On some Ostrowski type inequalities via montgomery identity and Tailor's formula显示文摘 | Aljinovic A A Pecaric | 2005 | Tamkang Journal of Mathematics2005，36，3： | 1 |
| 5 | The guadalupian (Permian) Kamura event in European Tethys显示文摘 | Isozaki Y Aljinovic' D Kawahata H | 2011 | Palaeogeography Palaeoclimatology Palaeoecology2011，308，12： | 1 |
| 6 | Stratigraphy of Upper Permian and Lower Triassic Strata of the Ziri Area ( Slovenia ) 显示文摘 | JURKOVSEK T K JURKOVSEK B ALJINOVIC D GALINA P | 2011 | Geologija2011，542，： | 1 |
| 7 | Failure of bulk bone grafts after total hip arthroplasty for hip dysplasia显示文摘 | Domagoj Delimar Ana Aljinovic Goran Bicanic | 2014 | Archives of Orthopaedic and Trauma Surgery2014，，8： | 1 |
| 8 | Western Tethyan Epeiric Ramp Setting in the Early Triassic: An Example from the Central Dinarides (Croatia)显示文摘In the central part of the External Dinarides in Plavno, Croatia, near Knin, a remarkably thick(927.5 m) Early Triassic depositional sequence was investigated. The Plavno sequence starts in the Early Griesbachian and ends with a continuous transition into the Anisian strata. A complete 13 C isotope curve has been achieved and combined with conodonts, bivalves and ammonoids to establish and correlate stage and substage boundaries. The δ13 C curve is consistent with former studies. It displays a general increase from the Griesbachian to a prominent maximum beyond the +8‰ amplitude around the Dienerian-Smithian boundary(DSB), followed by a steep and continuous decline to low, negative values in the Smithian. Around the Smithian-Spathian boundary(SSB) a steep rise to a second maximum occurred. It is followed by a saw-tooth shaped decline in the Spathian and a similar increase to a peak at the Spathian-Anisian boundary(SAB). Sedimentologically, the Plavno sequence is interpreted as having been deposited on an extensive epeiric ramp under long-term transgressive conditions, sharing depositional characteristics of both the epeiric platform and the carbonate ramp. The entire Plavno sequence was deposited above the storm-wave base and was storm influenced. Three informal members are differentiated: 1) the dolostone member(Early Griesbachian); 2) the siliciclastic member(red-coloured shale, siltstone, sandstone with oolitic/bioclastic grainstone intercalations), which can be further divided into lower, middle and upper intervals(Late Griesbachian, Dienerian and Smithian); and 3) the mudstone member(grey lime mudstones, marls and calcisiltites with common ammonoids and gastropods-Spathian). The Plavno sequence is compared with other western Tethyan sections. Observed differences stem from local controls on deposition in the overall shallow marine environment. | Dunja Aljinovic Micha Horacek Leopold Krystyn Sylvain Richoz Tea Kolar-Jurkovsek Duje Smircic Bogdan Jurkovsek | 2018 | Journal of Earth Science2018，29，4： | 1 |
| 9 | The occurrence of giant bivalve Alatoconchidae from the Yabeina zone (Upper Guadalupian, Permian) in European Tethys显示文摘 | Aljinovic' D Isozaki Y Sremac J | 2008 | Gondwana Research2008，13，3： | 1 |
| 10 | End-Guadalupian extinction of the Permian gigantic bivalve Alatoconchidae: end of gigantism in tropical seas by cooling显示文摘 | Isozaki Y Aljinovic' D | 2009 | Palaeogeography Palaeoclimatology Palaeoecology2009，284，12： | 1 |
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