查詢結果分析
來源資料
相關文獻
- Miocene Series and Its Basement Strata in Taimali-Tawu Area Southeastern Taiwan
- 臺南盆地之基盤構造與漸新世至中新世地層研究
- Upper Miocene Stratigraphy and the Horizon of Post-Lushanian Faunal Turnover in Northeastern Taiwan
- 臺灣北港地區下部中新統之孢粉生物地層與油氣潛能
- 臺灣北部中新統電測地層因素函數之確定
- Calcareous Nannofossils of the Subsurface Pre-Miocene Rocks from the Peikang Basement High and Adjacent Areas in Western Central Taiwan (Part 2: Paleocene)
- Stratigraphy and Sedimentology of the Miocene in Western Taiwan
- Calcareous Nannofossils of the Subsurface Pre-Miocene Pocks from the Peikang Basement High and Adjacent Areas in Western Central Taiwan (Part 1: Cretaceous)
- 苗栗地區打鹿砂層的沈積環境與地層架構
- Relative Sea-Level Changes in Oligocene to Miocene Strata in Northern Taiwan: A Preliminary Study
頁籤選單縮合
題名 | Miocene Series and Its Basement Strata in Taimali-Tawu Area Southeastern Taiwan=太麻里、大武地區之中新統及其基盤地層 |
---|---|
作者姓名(中文) | 顏滄波; 楊玉同; | 書刊名 | 中國地質學會會刊 |
卷期 | 34:1 1991.01[民80.01] |
頁次 | 頁3-16 |
分類號 | 352.65 |
關鍵詞 | 大武; 中新統; 太麻里; 地層; 基盤; |
語文 | 英文(English) |
中文摘要 | 本文是在下坡運動(mass wasting)較發達的沉積岩地區,以各露頭的岩型組合資料暫時加以地層學的考察為主。參考已有的有化石研究考察河底出露岩石的時代問題。又全地層的沉積時代問題要等更多的沉積學及古生物學研究後似才能明瞭。從恆春半島全域的地表地質推測地下或地殼上部的巨視地質,然後再檢討本地區的初步布蓋重力圖及磁力圖。太麻里.大武地區的中新統主由頁岩、板岩質頁岩、砂岩構成,而在主要河流底時含有有孔蟲帶N8的化石,在北部有N7石化出現(張麗旭,一九七○年)。中新統的基盤岩層主由片狀砂岩、板岩、片岩、結晶石灰岩、石灰岩等構成,而其時代似為始新世、中生代及古生代晚期。中新統與其基盤岩層間有一顯著的不整合關係。布蓋重力圖及磁力圖暗示太麻里、大武地區與枋寮、枋山地區間在淺部地殼的地質上有些差異的存在地表地質推測兩地區屬於同一個較平緩的大複背斜構造,各位於其東翼及西翼部份。 |
英文摘要 | The Miocene series in the Taimali-Tawu area consists mainly of shale, slaty shale and sandstone, and in places contains the early and middle Miocene foraminifers (zones N8 to N7 or older/younger) with definite N9 indicators. The basement strata under the Miocene series are compose chiefly of schistose sandstone, slate, crystalline schists, crystalline limestone and limestone, and may range from Eocene to Mesozoic-late Paleozoic in age. Between the Miocene series and its basement strata, there is a significant unconformity. The gravity and magnetic patterns show that the Taimali-Tawu area and the Fangshan-Fangliao area, occupying the east and west limbs of an anticlinorium respectively, are different in geologic features such as thickness of the Miocene series, depth of the basement strata, shallow geologic structure, etc. |
本系統之摘要資訊系依該期刊論文摘要之資訊為主。