BH250-50

Title

BH250-50

Subject

Duluth Gabbro

Description

Major Mineral: anorthite, orthopyroxene, clinopyroxene, olivine
Minor Minerals: oxides, biotite

The Duluth Gabbro, also known as the Duluth Complex, is a large, layered mafic intrusive body located in northeastern Minnesota, USA. It is part of the Midcontinent Rift System and is one of the most studied examples of Proterozoic layered intrusions in North America. Several BH250 samples belong to this gabbro, including BH250-11, 50, 189, 192, and 193.

This gabbro is globally recognized as a classic example of a layered mafic intrusion, and the term Duluth Gabbro / Duluth Complex is widely used in both academic and geological literature. It is approximately 1.1 billion years old (Mesoproterozoic).

Mineralogy:
Major minerals (vary by zone):
Plagioclase feldspar: Predominantly labradorite to bytownite (An50–An80)

Clinopyroxene: Mainly augite
Orthopyroxene: Common in more evolved layers, typically bronzite or hypersthene

Olivine: Present in the ultramafic base, ranging from forsteritic to fayalitic

Oxide minerals: Magnetite and ilmenite, especially abundant in oxide-rich zones

Accessory/Minor minerals:
Amphibole (e.g., hornblende, actinolite), especially in altered zones

Biotite and chlorite, commonly in more evolved or hydrothermally altered portions

Serpentine, typically associated with olivine alteration

Textures and Structures:
The Duluth Gabbro displays prominent layered cumulate textures, indicating crystal settling and magmatic differentiation within a large magma chamber.

Rhythmic layering, adcumulates, and mesocumulates throughout the complex point to open-system magmatic processes with periodic magma recharge.

These features are visible at numerous outcrops across the complex.

Geochemistry:
Compositionally mafic to ultramafic. Enriched in Fe, Mg, Ca, and Ti; depleted in Si and alkalis. Basal ultramafic rocks contain high concentrations of Cr and Ni, indicating early-stage cumulate formation. Rare Earth Element (REE) patterns show moderate Light REE (LREE) enrichment and negative europium (Eu) anomalies in some evolved units.




Coverage

Location: Duluth Vistor Center, Minnesota, USA
GPS Location: 46°43'46.78"N, 92°12'25.09"W

Creator

Bereket Haileab

Source

From the rock collection of Bereket Haileab. Sample 50. Housed at Carleton College in Minnesota.

Type

Thin section and hand sample

Relation


View on ArcGIS Online here






























TAS diagram of sample BH250-50.

Collection

Citation

Bereket Haileab, “BH250-50,” BH250 Mineralogy Teaching Collection, accessed April 25, 2026, https://bereket-haileab.geology.sites.carleton.edu/items/show/58.

Output Formats