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Crustal Reflectivity (Oceanic) and Magma Chamber

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Encyclopedia of Solid Earth Geophysics

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Synonyms

Melt lens; Spreading center and ridge

Definition

  • Axial magma chamber (Melt lens) is a thin melt lens observed at ocean spreading centers.

  • Layer 2A or Lava is the top layer of oceanic igneous crust.

  • Layer 2B is a dike sequence and lies above the axial melt lens.

  • Layer 3 (gabbro) forms the lower oceanic crust.

  • Moho is a boundary between the crust and mantle.

  • Pg is a seismic ray that travels through the crust.

  • PmP is a reflection from the crust–mantle boundary.

  • Pn is a ray that travels in the upper mantle.

  • Tomography is a technique to image the velocity structure of the earth.

Introduction

Over 70% of the earth’s crust is formed by the cooling and crystallization of melt at ocean spreading centers, which represent over 55,000 km of chains of volcanoes in the middle of the oceans, called mid-ocean ridges. At ocean spreading centers, the oceanic plate separates causing the mantle to move upward, reducing the pressure and causing the melting of the mantle. Since the newly formed...

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Correspondence to Satish C. Singh .

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Singh, S.C. (2011). Crustal Reflectivity (Oceanic) and Magma Chamber. In: Gupta, H.K. (eds) Encyclopedia of Solid Earth Geophysics. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-8702-7_58

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