BH250-98

Title

BH250-98

Subject

Granite with Basaltic Dike

Description

Major Minerals: plagioclase, biotite
Minor Minerals: chlorite, clinopyroxene

A thin basaltic dike intruded into a granite host rock. Upon emplacement, the dike developed a chilled margin where the hot basaltic melt came into contact with the cooler granite. The flow direction of the melt is preserved along the chilled margin, where the alignment of plagioclase laths records the magma's movement. Toward the center of the dike, this flow fabric becomes indistinct, and grain size increases progressively from the margin inward—reflecting slower cooling rates away from the contact zone.

Two types of thin sections were prepared from this sample: a standard thin section and a large-format thin section that spans the entire width of the dike, from one granite contact, through the basaltic interior, to the opposite granite contact.

This rock, both in hand sample and thin section, was used for a class project in one of my introductory geology courses. Students measured grain size variations across the dike and analyzed textural transitions. The paper they produced as part of this assignment is attached at the bottom of the page.

Coverage

Location: Granite Falls, Minnesota, USA

Creator

Bereket Haileab

Source

From the rock collection of Bereket Haileab. Sample 98. Housed at Carleton College in Minnesota.

Type

Hand sample and thin section
Large thin sections 2-3 inches

Relation







 

Collection

Citation

Bereket Haileab, “BH250-98,” BH250 Mineralogy Teaching Collection, accessed April 25, 2026, https://bereket-haileab.geology.sites.carleton.edu/items/show/111.

Output Formats