• 자원환경지질
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• 제17권4호
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• pp.299-314
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• 1984

The Yeongdo Island in Busan City is a remnant of the latest Cretaceous volcano, and consists geologically of andesites, rhyolite tuff, pelitic and psammitic hornfelses, lapilli rhyodacite tuff of the Yucheon Group, felsite and felsite porphyry of the Bulgugsa intrusives, and Holocene sediments in ascending order. The hornfelses are bound to the Taejongdae Formation. The stratigraphic position of the Formation is determined definitely into the Yucheon Group, thus the geologic age is approximately the same with the volcanic rocks of the Group. The sediments had been thermally metamorphosed to make pelitic and psammitic hornfelses of the albite epidote hornfels facies by the effects of active hydrothermal circulation, vaporization, and hybridization of andesitic solution, or of basification of acidic intrusives. Thus, on occasion, those hornfelses are not used to be distinguished from the andesitic rocks in the southeastern part of the Korean peninsula. The paleocurrent direction determined from several cross-beddings of the Taejongdae Formation is suggested to be from southwest to northeast. Orbicular rocks occur in hornfelsed rhyolite tuff, pelitic- and psammitic-hornfelses, and felsite porphyry at a lot of outcrops in the area of southwestern shoreline of the Yeongdo Island. Orbicules in rhyolite tuff and hornfels in the island might have originated from diffusion processes of metasomatic metamorphism carried out by hydrothermal solution rised from the intrusive adamellite which may be emplaced deeply under the Yeongdo volcanics. Those orbicules are due to metasomatic, secondary, and epigenetic origin. Proto-, multi-shelled, and multi-cored orbicules are described in the orbicular tuff. But multi-cored orbicules are not found in the orbicular fornfels. 250 tuff-orbicules numbered sporadically are in $20,000m^2$ area of the locality of orbicular tuff. About 60 hornfels-orbicules occurred sporadically are in $1,700m^2$ area of the locality of orbicular hornfels in the Taejongdae Formation. Orbicules in felsite porphyry might have originated by diffusion reaction between xenoliths and a quiescent zone in felsite porphyry magma. Those are of igneous, primary, and syngenetic origin.

• 광물과 암석
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• 제34권4호
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• pp.293-311
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• 2021

부산광역시 남해안에 위치한 행정자치구 영도(Yeongdo island) 봉래산 일원을 구성하는 화산암류는 안산암질~유문암질암으로 구성된다. 안산암질암은 주로 화산각력암으로 구성되며, 반정으로 사장석을 가지며 다량의 암편(岩片)을 함유하고 있다. 유문암질암은 산출형태에 따라 봉래산 기저부는 화산각력암으로 구성되며, 용결응회암이 봉래산 주산체를 이룬다. 육안으로 피아메 구조를 관찰할 수 있고, 고도가 높아질수록 용결구조는 약하게 발달하고 응회암을 구성하는 암편 및 결정 함량은 적어진다. 본 연구지역을 형성한 마그마는 섭입작용과 관련된 대륙연변부의 조구조 환경과 관련 있으며, 약간의 대륙지각의 혼염과 동시에 분별결정작용을 겪은 뒤 분출하였음을 지시한다. 고도별 주원소를 분석한 결과, 최소 4회 이상의 마그마 배취(magma batches)가 주입되어 혼합이 일어난 결과로 생각된다.

• 한국항해항만학회지
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• 제33권3호
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• pp.241-245
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• 2009

도심지의 열섬(Heat Island)현상과 연안지역의 해풍(海風)의 영향 때문에, 부산, 인천, 목포 등 연안도시의 도심지역과 연안지역의 각 외기 상태가 서로 다르게 나타난다. 이러한 외기조건은 건물의 냉방부하, 난방부하, 전력소비량 등에 직접적인 영향을 미치기 때문에, 에너지절약을 위한 건물설계와 운전방법개발을 위해서는 각 지역에 위치한 건물의 에너지소비특성을 파악해야만 한다. 본 연구에서는 연안지역 아파트의 전력소비량에 주목하였고, 부산광역시 영도구에 위치한 세대수가 100세대 이상인 22개 아파트 단지를 대상으로 기간별, 기능별 전력소비량을 조사하였다. 22개 아파트 전체의 세대내 최대전력소비량은 8월에 발생하고 있으나, 공용 최대전력소비량은 1월에 발생하고 있음을 알수 있었다. 한편 연안지역에서는 여름철에 해풍에 의한 자연환기로 인해 냉방용 전력소비가 감소할 것으로 예상하였으나, 조사결과에서는 여름철에 최대부하가 발생하였는데, 이는 해풍에 포함된 염분의 피해를 예방하기 위해 창문을 닫고 전기구동 에어컨으로 냉방하기 때문인 것으로 파악되었다.

• 기술사
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• 제27권6호
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• pp.72-84
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• 1994

This is about an environmental study of groundwater interference by hydrodynamic dispersion between the well A and well C in Dongsam-dong, the Yeongdo Island, Pusan, Korea. The groundwater in the study wells come from the fracture zones deeply seated in welded lapilli rhyodacitic tuff of the Late Cretaceous Yucheon Group. The boring depth at the well A is 190 meters, and the optimal pumping rate of the well A is about 100 cubic meters per day therein. The fractured aquifers in impermeable welded tuff show the conjugate fracturing type and are of anisotropic. The aquifers along two fracture zones in the well A are 80 and 100 meters in depth, respectively. It is not suggested that those fractured aquifers are simply connected between the well A and C. The sea level fluctuation by ebb and high tides in a day is not effective to the groundwater table in the well A. The pumping for 15 days at the well A doesn't give rise to any changes of the groundwater levels in the neighbor well C. The radius of influence of the well A is measured as less than 200 meters. The measuring electric conductivity for the test of salt tracer doesn't testify any relationship between the well A and the well C. There is the main difference between the well A and the well C on the basis of the water analysis of those wells. the well A is located in the high content zone of salt much over the standard value for drinking, whereas the other wells B. C. D are in the low content area of salt below the standard value. It is elucidated for the high content zone of salt in Yeongdo around the well A to have been uplifted over 20 meters.