THE INTENSITY OF INDONESIAN THROUGHFLOW (ITF) DURING THE HEINRICH STADIAL 1 PERIOD IN THE MAKASSAR STRAIT USING PLANKTONIC FORAMINIFERA APPROACH
The Heinrich Stadial 1 (HS 1) was a deglacial event in the North Atlantic that occurred approximately 18,000 to 15,000 years ago. During this period, there was a reduction in the volume of warm tropical surface water flow to the North Atlantic such that heat accumulated in the Southern Hemisph...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/85183 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |