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The Rock of The Lamongan Volcano.

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In accordance with Lorie and Prof. Behrens we have determined all collected samples as real basalts. The microscopic praeparates only show difference in relative number and size of the separated crystalls between them, and with respect to the groundmass, also in his capacity of the groundmass itself. As conson with basalt, the olivine exclusively appears as porphyric separation and not in the groundmass; augite on the contrary mainly occurs in the groundmass, alhough the cases are also not seldom, that great augitos occur porphyrically. The pyroxene belongs always exclusively to the monocline variety, the rhombie onen are absent.

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Ketersediaan

Informasi Detail

Judul Seri

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No. Panggil

PVG E.086-1

Penerbit

Bandung, Jawa Barat, Indonesia : Pusat Vulkanologi dan Mitigasi Bencana Geologi., 1886

Deskripsi Fisik

4 hml

Bahasa

English

ISBN/ISSN

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Klasifikasi

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Tipe Isi

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Tipe Media

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Tipe Pembawa

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Edisi

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Subjek

Volcano
Rocks
Gunung Lamongan

Info Detail Spesifik

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Pernyataan Tanggungjawab

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Informasi Lainnya

Kode Wilayah

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Pulau Dan Lembar Peta

Lainnya

Provinsi

Jawa Tengah

Koordinat - Latitude

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Koordinat - Longitude

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Versi lain/terkait

Lampiran Berkas