2020年1月4日 星期六

馬屎洲地質考察

  1. 馬屎洲地質考察地點 http://www.arcgis.com/home/webmap/viewer.html?webmap=3a637c064fb34c9d8849459ba81cb4e7
  2. GEO PARK LEAFLET https://www.geopark.gov.hk/eleaflet/pdf/07-E-leaflet-Ma-Shi-Chau.pdf
  3. HKU https://web.hku.hk/~chanls/Teaching_Resources/fieldTripGuides/ma%20sze%20chau%20_EDB.pdf
  4. HONG KONG GEOLOGICAL HISTORY https://www.edb.gov.hk/attachment/en/curriculum-development/kla/pshe/references-and-resources/geography/VolcanicGeology.pdf

The Geological Stratigraphy in the Northwestern Ma Shi Chau Hardcover – 26 January 2017

This dissertation, "The Geological Stratigraphy in the Northwestern Ma Shi Chau" by Shing-cheong, Francis, Law, 羅承昌, was obtained from The University of Hong Kong (Pokfulam, Hong Kong) and is being sold pursuant to Creative Commons: Attribution 3.0 Hong Kong License. The content of this dissertation has not been altered in any way. We have altered the formatting in order to facilitate the ease of printing and reading of the dissertation. All rights not granted by the above license are retained by the author.


Abstract:
Before the year 2000, the sedimentary and volcano-sedimentary rocks on Ma Shi Chau (MSC) have long been regarded as the formations in Permian and Jurassic respectively. Geotechnical Engineering Office (GEO) had modified the geological model and changed the Northeastern side of MSC, the pre-volcanic sedimentary rocks, to an older rock formation, from Permian Tolo Harbour Formation to Devonian Bluff Head Formation. The reasons of change are mainly from structural evidence and lithological evidence.

But they are still indirect evidences; no fossil was found in the sedimentary sequences at the hinging wall till to the northwestern shore of Ma Shi Chau. Fossils were only found along the southeastern shore of Ma Shi Chau for the footwall of the reverse fault, which are of Permian age.

Through the analysis of the photomicrographs, the Unknown group is difficult to show which formations, the Devonian or Permian is closer to as the Unknown group have similar characteristics of both. For the geochemistry analysis by using different graphs, the patterns of each group are revealed.

From the graphs produced, generally the Unknown group have pattern closer to the Permian Tolo Harbor Formation. But there is still no direct evidence that the Unknown group is within the Permian Tolo Harbor Formation. By the geochemical data it is more likely for the Unknown group to be close the Permian rocks.

DOI: 10.5353/th_b5094852
Subjects:
Geology, Stratigraphic
Geology - China - Hong Kong

AFCD

地質公園土地利用的爭議
































沒有留言:

張貼留言

精選文章

夏日維京:挪威 DAY 1

挪威奧斯陸 (OSLO) ~~~~~~~~~ 今日由芬蘭赫爾辛基到挪威奧斯陸。我們住在經濟實惠的Citybox Oslo,一出火車站左面第二條直街,我們住在頂樓還有天窗呢! 雖然已是七月中旬,下微微雨,冷冰冰的空氣加入雨...