We apply 2-D wave-equation prestack depth migration to a North Sea basalt dataset. High velocity and impedance contrasts across a basalt layer causes low P-wave reflection signal-to-noise ratio under the basalt. We first migrate the P-wave data with a provided depth velocity model, and then replace sub-basalt P-wave velocity with a simple estimate of shear wave velocity and migrate locally-conv...

The proposal by Hubbard et al. (1) that "Very High Alumina basalt" ("VHA basalt") may represent an important primary lunar magma type neglects consideration of certain well-characterized high-magnesium highland rocks, among them spinel troctolite from Luna 20 (2) and Apollo 16 samples (3) and dunite from Apollo 17 samples (4), and the possibility that "VHA basalt" may in fact have originated by...

The paper presents two experimental methods for basalt processing by microwaves, and their results. One method employs a single-mode cavity to melt basalt, and to produce a volcanic glass (obsidian). The other method uses an open-end applicator (i.e. a microwave drill [1]) to form holes in basalt rocks. Experimental observations of the basalt interactions with microwaves in these two schemes ar...

Ferroan anorthosite VHK basalt Oldest basalt APOLLO 14 OLDEST MARE BASALT REVISITED: POSSIBLE PETROGENETIC CONNECTION BETWEEN MG GABBRONORITE AND VHK BASALT. T. Arai, H. Takeda, M. Miyamoto, and H. Kojima, Antarctic Meteorite Research Center, National Institute of Polar Research, 1-9-10 Kaga Itabashi Tokyo 173-8515, Japan, [email protected], Research Institute, Chiba Institute of Technology, Ts...

Late Oligocene (ca 25 Ma) volcano-sedimentary successions exposed on the western periphery of Doupovské Hory Volcanic Complex reveal a complex sedimentation history influenced in various ways by decay alkali basalt volcanic edifice. Weathering rocks supplied abundant reactants that promoted carbonate precipitation peripheral palaeolakes—as evidenced strongly non-radiogenic 87Sr/86Sr values (0.7...

In the previous paper, geological ages of Late Cretaceous, Paleocene, late Middle to Eocene, Oligocene and early Early Miocene were confirmed at first time, based on occurrences both age diagnostic larger foraminifera associated planktonic foraminifera, from Sashida Limestone included basalt pebbles, Sashida, Kamo-Gun, south Izu Peninsula. Therefore, was made up clastic carbonate rocks various ...