• Journal of the Korean Arthroscopy Society
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• v.12 no.3
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• pp.185-190
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• 2008

Purpose: The purpose of this study is to provide the clinical outcomes of arthroscopic type II SLAP repair in non-athletes, and to compare the clinical outcomes between those who had isolated type II SLAP lesion and those who had combined partial thickness supraspinatus tear that did not required a combined repair. Materials and Methods: From July 2005 to January 2007, 142 consecutive type II SLAP lesions were treated with arthroscopic surgery. The inclusion criteria for the study were; (1) younger than 50 years old; and (2) non-athletes. Exclusion criteria were; (1) prior surgery, fracture or combined recurrent dislocation history on the affected shoulder; (2) combined full thickness rotator cuff tear or PTST (>50% thickness) patient that needed repair; and (3) combined infection, arthritis or inflammatory disease. Remaining 19 patients meet the criteria. Among them, 13 had combined PTRCT that did not require repair (Group I), and 6 had isolated type II SLAP lesion without combined supraspinatus tear (Group II). The mean age was 36.7 years (29~49 years), mean symptom duration was 39.1 months (3~216 months) and mean follow-up was 19.0 months (12~27 months). In all patients, the range of motion of affected shoulder, pain and function visual analogue scale (PVAS, FVAS), the Constant score and UCLA score were evaluated preoperatively and postoperatively. Results: In group I, external rotation at side was decreased significantly (p=0.003),but there were no statistical significant change at the remains(p>0.05). And there were no differences between groups (p>0.05). At the final follow-up, all clinical outcome measurements improved after surgery with statistical significance (p<0.05): UCLA score, $22.8{\pm}5.2$ to $32.8{\pm}2.1$; Constant score, $79.4{\pm}8.6$ to $94.9{\pm}4.3$; PVAS $5.4{\pm}2.7$ to $1.1{\pm}1.4$; FVAS $63.2{\pm}15.3$ to $93.4{\pm}7.3$. But, in group comparison of the mean UCLA score and Constant score, there were no statistical significant differences between two groups. Conclusion: Arthroscopic repair of type II SLAP lesion provided good clinical outcomes in nonathletic population. Combined partial thickness supraspinatus tear does not seem to hamper the final outcome at minimal 1 year follow-up.

• Journal of the Korean earth science society
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• v.21 no.4
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• pp.449-468
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• 2000

The Ordovician Chongson Limestone deposited in the carbonate ramp to the rimmed shelf shows diverse diagenetic features. The marine diagenetic feature appears as isopachous cements surrounding ooids and peloids. Meteoric diagenetic features are recrystallized finely and coarsely crystalline calcite, evaporite casts filled with calcite, and isopachous sparry calcite surrounding ooid grains. Shallow burial diagenetic features include wispy seam, microstylolite, and dissolution seam whereas deep burial features include stylolite, burial cements. blocky calcite with twin lamellae, and poikilotopic calcite. Dolomites consist of very finely to finely crystalline mosaic dolomite formed as supratidal dolomite, disseminated dolomite of diverse origin, patchy dolomite formed from bioturbated mottles, and saddle dolomite of burial origin. Silicified features include calcite-replacing quartz and fracture-filling megaquartz. Burial cements characterized by poikilotopic texture show ${\delta}^{18}$O value of -10.4 %$_o$ PDB, ${\delta}^{13}$C value of -1.0%$_o$ PDB and 504ppm Sr, 3643ppm Fe, and 152ppm Mn concentrations. Finely and coarsely crystalline limestones show similar ${\delta}^{18}$O and ${\delta}^{13}$C value to those of burial cements; however, they show lower Sr and higher Fe and Mn concentrations than burial cements. This suggests that very finely and coarsely crystalline limestones were recrystallized in freshwater and then they were readjusted geochemically in the burial setting whereas the burial cements were formed in relatively high temperature and low water/rock ratio conditions. Very finely and finely crystalline mosaic dolomites with ${\delta}^{18}$O value of -8.2%$_o$ PDB, ${\delta}^{13}$C value of -1.9 %$_o$ PDB, and 213ppm Sr, 3654ppm Fe, and 114ppm Mn concentrations, respectively are interpreted to have been formed penecontemporaneously in supratidal flat and then recrystallized in the low water/rock ratio burial environment. Geochemical data suggest that the low water/rock ratio burial environment was the dominant diagenetic setting in the Chongson Limestone. The Chongson Limestone has experienced marine and meteoric diagenesis during early diagenesis. With deposition of Haengmae and Hoedongri formations part of the Chongson Limestone was buried beneath these formations and it experienced shallow burial diagenesis. During the Devonian the Chongson Limestone was tectonically deformed and subaerially exposed. During the Carboniferous to the Permian about 3.3km thick Pyongan Supergroup was deposited on the Chongson Limestone and the Chongson Limestone was in deep burial depths and stylolite, burial cements, blocky calcite and saddle dolomite were formed. After this burial event the Chongson Limestone was subaerially exposed during the Mesozoic and Cenozoic by three periods of tectonic disturbance including Songnim, Daebo and Bulguksa disturbance. Since the Bulguksa disturbance during Cretaceous and early Tertiary the Chongson Limestone has been subaerially exposed.