• Sleep Medicine and Psychophysiology
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• v.16 no.1
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• pp.28-35
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• 2009

Introduction: Human attachment is known to be closely associated with psychophysiological phenomenon. However, there have not been enough researches on the relationship of the attachment with sleep, especially with insomnia. The objective of the present study was to investigate the relationship between adult attachment styles and insomnia in community-dwelling population. Methods: One hundred seventy seven community-dwelling adults (74 males and 103 females；mean age $41.23{\pm}8.44$) participated in the current study. To assess the attachment styles (secure, dismissing, preoccupied and fearful), self-reporting Relationship Style Questionnaires (RSQ) were completed by the participants. Presence, type, frequency and duration of insomnia in the last month were also investigated. Results: Compared to subjects without insomnia, subjects with insomnia had higher fearful attachment scores (t=2.87, p=0.005). Higher fearful attachment score were found in all subtypes of insomnia (sleep-onset insomnia, t=2.33, p=0.021；maintenance insomnia, t=2.92, p=0.004；terminal insomnia, t=2.89, p=0.004). Subjects with frequent (${\ge}3$ per week) insomnia had higher fearful attachment scores than subjects with infrequent (${\le}2$ per week) insomnia (t=2.57, p=0.012). In addition, subjects with chronic insomnia (${\ge}6$ months) had higher preoccupied attachment scores relative to subjects with transient insomnia (<6 months), (t=2.57, p=0.012). Conclusion: In the current study, attachment styles were different depending on the characteristics of insomnia. The fearful attachment was associated with the presence of insomnia, while the preoccupied attachment was associated with the chronicity of insomnia. These findings suggest that there may be some relationship between the adult attachment styles and the clinical features of insomnia.

• Economic and Environmental Geology
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• v.12 no.2
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• pp.51-73
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• 1979

The zinc-lead deposits at the Yeonhwa I mine were investigated in terms of ore-forming geologic setting, structural style of ore control, geometry of individual orebodies, zoning, paragenesis and chemical composition of skarn minerals, as well as metal grades and ratios of selected orebodies. The Yeonhwa I mine is characterized by a large swarm of chimney type massive orebodies with thin skarn envelopes, boldly developed through a thick sequence of Pungchon Limestone, the overlying Hwajeol Formation, and the underlying Myobong Slate of Cambrian age. Nearly 20 orebodies of similar shape, but of varying size are arranged in a V-shaped pattern with northwest and northeast trends, clearly indicating an outstanding ore control by a conjugate system of fractures with these trends. Important orebodies are the Wolam 1, 2, 3, and 5 orebodies in the west, and the Namsan 1, 2, 3. and 5 orebodies in the east, among others. The Wolam 1 orebody, which was observed from the -360 level through the -240, -120, and 0 levels to the surface outcrops (totaling a vertical height of about 500m), shows a vertical variation in skarn mineralogy, ranging from pyroxene-garnet zone on the lower levels. through pyroxene (without garnet) zone on the intermediate levels, and finally to rhodochrosite vein on the upper levels and surface. Microprobe analyses of pyroxene and garnet on a total of 14 mineral grains revealed that pyroxenes are manganoan salitic in most samples, with downward increase of Fe and Mn, whereas garnets are highly andraditic, containing fractions of subordinate grossular with downward decrease of Fe. This indicates a reverse relationship of Fe-contents between pyroxene and garnet with depth. Ore minerals are major sphalerite, subordinate galena, and minor chalcopyrite. Sulfide gangue minerals include major pyrrhotite, and minor pyrite and marcasite of later age. Two types of variational trends in metal grades and ratios with depth are present on the plots of assay data from the Wolam orebodies: one is a steady upward increase in Pb, Zn, and Pb:Zn ratios, with a terminal decline at the top of orebody: the other is an irregular or sinusoidal change. The former is characteristic of chimney-type orebodies, whereas the latter is of vein· shaped orebodies. The Pb grades show large variations among orebodies and from level to level, whereas the Zn grades are relatively constand or less variable.