Skip to main content
Book Chapter

Geological History and Transition of the Biota of Lake Biwa

Springer International Publishing, (2020), 1-2
DOI: 10.1007/978-3-030-16969-5_1
0Citations
Citations of this article
1Readers
Mendeley users who have this article in their library.
Get full text

Abstract

The Lake Biwa area is one of the most active Cenozoic tectonic regions of the Japanese islands. District-wide geological structures and a large depressional basin are recognized in this area. The formation and development of the lake were controlled by fault movements that occurred through the Pliocene and Pleistocene epochs of the Cenozoic era.

Cite

CITATION STYLE

APA

Takahashi, K. (2020). Geological History and Transition of the Biota of Lake Biwa. In Lake Biwa: Interactions between Nature and People: Second Edition (pp. 1–2). Springer International Publishing. https://doi.org/10.1007/978-3-030-16969-5_1

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free