Exp 349: South China Sea Tectonics

Title: South China Sea Tectonics

Dates: 26 January to 30 March 2014

Ports: Hong Kong to Keelung

Co-chief Scientists: Chun-Feng Li & Jian Lin

Staff Scientist: Denise Kulhanek

Logging Staff Scientist: Trevor Williams (you can follow his blog for the Lamont/Columbia Earth Institute)

Expedition 349: South China Sea Tectonics will explore the formation of the South China Sea, a marginal sea in the Western Pacific located south of China and between the Philippines in the east and Vietnam in the west.

During the expedition we will core and log three sites into the oceanic basement, which is composed of volcanic rocks (primarily basalt) that form as molten rock cools. This molten material rises to the surface from deep within the Earth at mid-ocean ridges. As new rock forms along the mid-ocean ridge, older rock is pushed away from the ridge, making the ocean basin larger over millions of years. Previous studies examining the South China seafloor magnetic anomoloies (the record of the orientation of the Earth's magnetic field at the time the rocks formed) and other data collected during shipboard oceanographic surveys, suggest that the South China Sea began to form during the Oligocene (~32 million years ago) and stopped spreading during the early Miocene (~16 million years ago). The only way to test these age estimates is to drill into the South China Sea basement to obtain samples of fresh basalt to date using radiometric dating techniques.

To reach the oceanic basement at each of our sites, we will have to core through a lot of sedimentary rock that has been deposited on top of the basalt. These sedimentary rocks are mostly formed from the remains of organisms that lived in the ocean, died and fell to the seafloor, adn then became fossilized, as well as sand, silt and clay that enter the oceans through rivers. Studying these sediments will help scientists to better understand how climate has evolved in the southeast Asia region since the South China Sea started to form ~32 million years ago.

Primary goals of the expedition:

  1. Date the timing of the opening of different parts (sub-basins) of the South China Sea by coring oceanic basement rocks. We will use radiometric dating techniques to determine when these rocks formed. In addition, we will use the ages of the fossils (biostratigraphy) and magnetostratigraphy in the sediment lying directly on top of basement to help constrain the age of the rock below.
  2. Measure the physical properties, magnetization, and geochemical composition of basement rocks from different sub-basins of the South China Sea to understand why the magnetic anolomaly patterns are so different between the different sub-basins.
  3. Measure the geochemical and isotopic composition of basement rocks to better understand the mantle processes that formed the South China Sea.
  4. Study the age, composition and physical properties of the sediment and fossils deposited on top of the South China Sea basement to understand how the regional cimate responded to the formation of the South China Sea. We also want to develop a sedimentation model to better understand where the sediment found in the South China Sea comes from and how deposition of the sediment shaped the ocean basin.







South China Sea
United States
15° 22' 30" N, 117° 0' 0" E