STUDI BIOFASIES FORAMINFERA BESAR DI BATUAN KARBONAT FORMASI RAJAMANDALA BERUMUR OLIGOSEN AKHIR-MIOSEN AWAL DAERAH PADALARANG, JAWA BARAT
The Rajamandala Formation in Padalarang, West Java consists mostly of limestone that was deposited during Late Oligocene to lower part of Early Miocene age. This formation contains organism mainly larger foraminifera, coral and algae which need specific ecological condition to grow. In this st...
Saved in:
| 主要作者: | |
|---|---|
| 格式: | Theses |
| 語言: | Indonesia |
| 主題: | |
| 在線閱讀: | https://digilib.itb.ac.id/gdl/view/72914 |
| 標簽: |
添加標簽
沒有標簽, 成為第一個標記此記錄!
|