缺。
全球海水面約於 6 千年前達到相對穩定的階段，此時期的盆地下陷速率保持 穩定，沉積物供應的速率增加則使河口灣逐漸被填滿，豐富供應的沉積物使得盆 地中的河口灣約於 7 ka 即開始回填變淺，沉積環境逐漸回復到曲流河相，呈現類 似現今環境的樣貌。
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沉積環境的分析，西太平洋地質科學，第6 期，第 59-86 頁。
劉平妹，郭兆敏，曾美惠，蕭承龍，2006，台北盆地的孢粉層序及古氣候，西太
期九十三年度水文地質調查研究計畫，經濟部中央地質調查所，新北市，
附錄 臺北盆地探井岩芯柱狀圖
89
所有探井柱狀圖所採用之圖紋與縮寫皆同圖 3.2。
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